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Thd U.C. System
for Producing
Healthy- ^
Container- Grown
Plants
UNIVERSITY OF CALIFORNIA
Edited by
KENNETH F. BAKER
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The U. C. System
for Producing Healthy
Container-Grown Plants
through the Use of Clean Soil,
Clean Stock, and Sanitation
Edited by KENNETH F. BAKER
PHILIP A. CHANDLER, RICHARD D, DURBIN, JOHN FERGUSON,
J. W. HUFFMAN, O. A. MATKIN, DONALD E. MUNNECKE, CHESTER
N. ROISTACHER, WARREN R. SCHOONOVER, and R. H. SCIARONI
UNIVERSITY OF CALIFORNIA DIVISION OF AGRICULTURAL SCIENCES
AGRICULTURAL EXPERIMENT STATION— EXTENSION SERVICE
THIS MANUAL is one of a series published by the University of California College of
Agriculture and sold for a charge which is based upon returning only a portion of the
production cost. I>\ this means it is possible to make available publications which, due to
relatively high cost of production, or limited audience, would otherwise be beyond the
scope of the College publishing program.
CONTENTS
Page
1. The U. C. System: a General Summary, by Kenneth F. Baker 3
The problems; the answers; the future.
2. Today's Nursery Problems, by Kenneth F. Baker 28
The industry; plant diseases; adopting the U. C. system.
3. Damping-off and Related Diseases, by Kenneth F. Baker 34
Dynamics and prevention of nursery diseases.
4. The Salinity Problem in Nurseries, by Warren R. Schoonover and R. H. Sciaroni 52
Nature; plant injury; cause; prevention.
5. The U. C.-Type Soil Mixes, by O. A. Matkin and Philip A. Chandler 68
Preparation and uses of soil mixes and fertilizers.
6. Components and Development of Mixes, by O. A. Matkin, Philip A. Chandler, and
Kenneth F. Baker 86
Selecting physical and chemical components; history.
7. Nitrogen in Nursery Soils, by O. A. Matkin and Philip A. Chandler 108
Types and utilization of nitrogen sources.
8. Heat Treatment of Soil, by Kenneth F. Baker and Chester N. Roistacher 123
Benefits; practical procedures; cost.
9. Principles of Heat Treatment of Soil, by Kenneth F. Baker and Chester N. Roistacher. ... 138
How soil is heated; factors in equipment design.
10. Equipment for Heat Treatment of Soil, by Kenneth F. Baker and Chester N. Roistacher. . 162
Selecting equipment; steam generators; fuel.
1 1. Chemical Treatment of Nursery Soils, by Donald E. Munnecke 197
Materials and methods; soil drenches.
12. Treatment of Nursery Containers, by Kenneth F. Baker, Chester N. Roistacher, and
Philip A. Chandler 210
Heat; chemicals; self-disinfesting containers.
13. Development and Maintenance of Healthy Planting Stock, by Kenneth F. Baker and
Philip A. Chandler 217
Significance; obtaining and maintaining stock.
14. Beneficial Soil Microorganisms, by John Ferguson 237
Types; activities; controlled colonization.
15. Importance of Variation and Quantity of Pathogens, by Richard D. Durbin 255
Variability; inoculum potential; longevity in soil.
16. Grower Experience with the U. C. System, by R. H. Sciaroni and J. W. Huffman 263
Report on 12 examples of 7 types of nurseries.
17. Mechanization and the U. C. System, by J. W. Huffman and R. H. Sciaroni 271
Steps in production; flow diagrams.
Appendix 285
References; glossary; weights and measures; sources of equipment,
materials, fungicides, and chemicals.
Index 307
THE U. C. SYSTEM
THE AUTHORS
Kenneth F. Baker, Professor of Plant Pathology, and
Plant Pathologist in the Experiment Station, Los
Angeles.
Philip A. Chandler, Principal Laboratory Technician,
Department of Plant Pathology, Los Angeles.
Richard D. Durbin, Senior Laboratory Technician,
Department of Plant Pathology, Los Angeles.
John Ferguson, former Research Assistant, Depart-
ment of Plant Pathology, Los Angeles; now at the
Soil and Plant Laboratory, Orange, California.
John W. Huffman, Assistant Agriculturist, Agricul-
tural Extension Ssrvice, Los Angeles.
O. A. Matkin, former graduate student in Horticul-
tural Science, University of California, Los Ange-
les; now at the Soil and Plant Laboratory,
Orange, California.
Donald E. Munnecke, Assistant Professor of Plant
Pathology and Assistant Plant Pathologist in the
Experiment Station, Los Angeles.
Chester N. Roistacher, Principal Laboratory Techni-
cian, Department of Plant Pathology, Citrus Ex-
periment Station, Riverside, California.
Warren R. Schoonover, Agriculturist, Agricultural
Extension Service, Berkeley.
R. H. Sciaroni, Associate Agriculturist, Agricultural
Extension Service, Half Moon Bay.
Aids in Adopting
the U. C. System
here are several logical steps in con-
sidering the adoption of the system,
whether in converting an old nursery or
establishing a new one.
Decide whether the U. C. system for
producing healthy plants is to be adopted
in your nursery. The experiences of
twelve growers who have done so are
described in Section 16. The advantages
of such adoption are summarized on p.
30 through 33, 49, 51, and 270. If the
system is to be adopted, the cultural prac-
tices, present and contemplated, should
be surveyed on the following bases:
1. Compare the U. C.-type soil mixes
and nutrients with other possible soils on
the bases indicated in figure 65 and in
the related discussion in Section 6. A
summary may be found on p. 90, 93,
and 94.
2. The comparative ease of avoiding
salinity injury by methods outlined in
Section 4 should be studied for each of
the cultural systems considered.
3. Compare results with untreated soil
and that treated with heat or chemicals.
The experiences of the twelve growers
described in Section 16, and the benefits
reported on p. 49 and 51 show the neces-
sity of soil treatment.
4. Compare treatment of soil by chem-
icals and by steam to determine which
fits best into your operations. See table
13 and the accompanying discussion in
Section 8.
5. If steam is selected for soil treat-
ment:
a. The boiler size required for a given
amount of soil may be estimated from
table 14 and the discussion in Section 9.
b. The type of equipment best suited
for steaming in your nursery may be se-
lected by consulting table 15 and the data
in Section 10.
c. Possible ways to integrate such
equipment into the mechanization pro-
gram are shown in figure 126 and the
text of Section 17.
6. If chemicals are to be used for soil
treatment, the one best suited to your
needs may be determined through table
17 and the discussion in Section 11. Ways
to integrate such a treatment into a me-
chanization program are shown in figure
126 and the text of Section 17.
7. Possible methods for treating con-
tainers are discussed in Section 12.
Whenever possible, however, the soil
should be treated in the containers.
8. Pathogen-free stock or seed is neces-
sary. Methods for obtaining and main-
taining it are outlined in figure 115 and
in the text of Section 13.
9. Sanitary precautions necessary to
prevent contamination of clean soil and
stock are outlined in "A Nursery Sanita-
tion Code" in Section 1. The entire oper-
ation should be reviewed, step by step,
from the viewpoint of eliminating all
possible sources of contamination.
10. Some possibilities of mechaniza-
tion are presented in the flow diagram
(fig. 126) and in the accompanying text
in Section 17. Such a chart might well be
prepared for the contemplated plan. You
should also visit mechanized nurseries
and perhaps consult an engineer who
specializes in materials handling.
11. The technical assistance and ad-
vice of a well-trained person will reduce
errors and ease the transition while the
system is being adopted. In some coun-
[i]
ties your farm advisor will be able to stand why the various practices are per-
help during this "shake-down" period. formed. This manual should prove
12. The employees should be trained helpful in such training.
in the system used so that they under-
No endorsement of products or equipment referred to by trade names in this manual is intended, nor is
criticism implied of similar products which are not mentioned. No responsibility is assumed for commercial
soil mixes or fertilizers sold as formulations presented in this publication.
SECTION
The U.C. System:
A General Summary
The problems
The answers
The future
Kenneth F. Baker
.he most urgent need of the Califor-
nia nursery industry, within the limits of
its present market, is for lowered cost of
production. This is best achieved by re-
ducing plant losses and by lowering labor
cost through mechanization. These in
turn require modification of many exist-
ing practices. Production must be de-
pendable, uniform, and largely free from
unpredictable failures due to diseases,
salinity, insects, or weather.
The U. C. system of soil mixes, soil
and plant treatments, and handling op-
erations has been developed since 1941
by the Department of Plant Pathology,
University of California, Los Angeles,
to practically eliminate the principal
cause of such failure — diseases caused
by those organisms and factors which
involve the soil. It was evolved during
a time when mechanization was empha-
sized and, therefore, provides the neces-
sary adaptability and dependability for
the success of such a program. (Sec. 2.)1
1 These numbers in parentheses give the sec-
tion where further information on the topic
may be found.
Growers have generally found that
they can produce better plants faster,
easier, and more dependably by the U. C.
system than by previous methods. Conse-
quently many growers in California, as
well as in other areas, have adopted the
system or parts of it, and have contrib-
uted in turn to its development. The
large, year-round demand for nursery
stock in California has given added im-
petus to the program. The real key to the
development and adoption of the system,
however, has been the effective disease
and salinity control it has provided.
(Sec. 16.)
The magnitude of the over-all problem
is indicated by the quantity of soil used
by the California nursery industry each
year. It is estimated that this is about
350,000 cubic yards, or the top foot of
soil from 217 acres of land. (Sec. 2.)
Advances in disease control
There has been close parallel develop-
ment of disease-control practices in
plants and animals. Both have progressed
from superstitious practices, through the
[3]
use of antiseptics (on animals) and
sprays (on plants), to aseptic proce-
dures, to use of antibiotics (on animals
and plants) and retardant or antagon-
istic organisms (in soil). With plants
this has emphasized pathogen-free soil
and propagative material, and cultural
techniques to keep them that way. This,
the central core of the U. C. system, is
expressed in the motto, "Don't fight 'em,
eliminate 'em." (Sees. 3, 13, and 14.)
Successful prevention of a disease usu-
ally involves the application of more
than one treatment. For this reason, sev-
eral concurrent procedures are often sug-
gested for a given trouble in this manual.
Objective of this manual
The objective of this publication is to
assemble and synthesize information
from many sources into a unified plan
of action for nurseries. Many results of
our research are reported for the first
time. In addition, selected and tested in-
formation from many other sources has
been included to give a reasonably com-
plete picture up to January, 1957. This
manual is based on, and perhaps will
prove most useful to California nurseries,
but it should be helpful to growers in
other areas who have shown interest in
the U. C. system.
While specific recommendations of
present general application are made in
this manual, it is not a "cookbook" of
exact instructions. Nurseries vary so
widely in type, size, and location, and
in the number, kind, and age of crops
grown, that detailed recommendations
are often of limited application. Further-
more it is impossible to anticipate the
course of future developments in nursery
practice. If growers understand the sci-
entific bases underlying their practices,
they can adapt the system to their own
conditions and to future improvements
in methods and equipment. The dual
purpose of the manual, then, is to
provide a plan for present action, with
background information that will help
the grower shift with the improvements
that will surely come.
One of the principal uses of this
manual probably will be as a reference
work to look up some specific fact, and
the format has been arranged with this
in mind. A fairly complete index, num-
erous headings, frequent cross-refer-
ences, tabulated data, and a general
summary are provided. The same infor-
mation may appear more than once, in
order to reduce the danger that the refer-
ence user may acquire partial facts or
facts out of context. It has also some-
times been necessary to repeat points in
order to develop a line of reasoning. It
is hoped that the annoyance to the gen-
eral reader from such repetition will be
outweighed by its general utility.
THE PROBLEMS
Diseases
Diseases are a luxury
Nurserymen are coming to realize
that diseases are neither a necessary evil
nor a trivial factor in the gamble in-
volved in production of a crop. Diseases
are, in fact, important in determining The pathogens, and
what the grower does, how and when he n$Wtn«iy jsproad
docs it, and why. The viewpoint is gain-
ing acceptance that diseases are a luxury
modern nurseries can ill afford, because
I lies caii-c unnecessary losses. Because
of the trend toward crop specialization,
it is also well to remember that the fewer
the crops grown, the less can one afford
erratic disease loss in them. (Sees. 2
and 3.)
Damping-off (figs. 1, 12 through 18,
30, 33, and 34) and related diseases
(such as seed decay, top rot, cutting and
stem rot, and root rot of mature plants)
I 4
of nursery crops are most frequently
caused by Rhizoctonia solani, but also by
water molds (Pythium and Phytoph-
thora spp.). Less important are the cot-
tony-rot fungi (Sclerotinia sclerotiorum
and S. minor) and the gray mold (Bo-
trytis cinerea) , as well as host-special-
ized parasites, such as the aster-wilt Fu-
sarium. (Sec. 3.)
The losses caused by a disease are de-
termined by the interaction of several
factors: (1) the susceptibility of the
host, as well as its carbohydrate-nitrogen
status, and the vitality of the seed
planted; (2) the abundance (inoculum
potential)2 and virulence of the patho-
gen in the soil; (3) the favorableness of
the environment (for example, the levels
of salinity, moisture, and temperature in
the soil, the light available to the plant,
the depth of planting). (Sec. 3.)
The destructive Rhizoctonia and water
molds produce no important air-borne
spore stage, and their spread is, there-
fore, largely dependent on the scattering
2 Many of the technical terms used in this
manual are explained in the Glossary (p. 298).
CAUTION:
Many
of
the <
:hemicals
mentioned
in this
manual
are
poi-
sonous and
may
be
harmful.
The
user should
carefu
lly
Follow the
pre-
cautions on
the 1
abe
Is of
the
con-
tainers.
of soil or plant fragments in which they
are present. Spores of the water molds
may be spread in water stored in a tank
or reservoir, but not in that from city
mains or wells. Spread of any of these
fungi may occur when:
1. Soil is spattered by drops or a jet of
water, as from irrigation or rain;
2. The pathogen is spread by dipping
cuttings in water or in hormone
solutions;
3. Soil gets in the end of the hose when
it is dropped on the ground, and
is expelled into the bench with the
next watering;
4. Soil is carried over on flats, pots,
benches, or other containers be-
tween plantings;
Fig. 1. Rhizoctonia damping-off of pepper seedlings. Flat at left showing damping-off pro-
gressing inwardly from an infested container. Next to the flat the seedlings were infected first,
and rotted before emergence. Farther from the edge, the seedlings were successively bigger
before postemergence damping-off occurred. At right is shown the wire-stem phase of damping-
off (see arrow) of large seedlings, causing the plants to fall over.
Fig. 2. Which is the most important leg of a
three-legged stool?
5. Soil is carried over on tools, cloth
covers for flats, and on workmen's
hands;
6. The grower walks over treated soil or
flats;
7. Flats are placed on infested ground;
8. Infected seed, cuttings, or seedlings
are planted.
Therefore, emphasis in control is placed
on clean soil, clean stock, and sanitary
procedures to keep them that way (fig.
2 ) . Once the pathogen has penetrated
into a plant it is not economically pos-
sible to eradicate it except, with valuable
planting stocks, by heat treatment. (Sec.
13.) Chemical treatments generally are
ineffective. For these reasons prevention
is emphasized in plant disease control,
rather than cure, as in medical pro-
cedures. (Sec. 3.)
These fungi are not
restricted to juvenile plants
Fungi which cause damping-off and
related seedling diseases may kill a tree
or shrub some years later when the loss
is greater, or may infest for all time a
clean piece of ground. This fact imposes
on nurserymen the obligation to produce
plants free of disease organisms, rather
than merely free of symptoms. Cultural
suppression of these soil fungi in the
nursery is only likely to postpone dis-
ease until later, costlier losses occur.
(Sec. 3.)
Two strains of one
species may differ greatly
There is a widespread misconception
that, because Rhizoctonia solani (or some
other microorganism) is naturally pres-
ent in a given soil, it is unimportant
whether more of it is introduced with
planting stock, soil, or manure. Evalu-
ating the similarities of the disease po-
tential of two organisms is a specialist's
job, and a grower can with safety only
assume them to be different until proved
otherwise, even though the same scien-
tific or common name is applied to them
or to the diseases they cause. Strains of
a single species may differ in: (1) the
hosts which they can attack (fig. 124) ;
(2) the virulence of attack (fig. 124),
which on a given host may range from
nonpathogenic to highly potent; (3) the
temperatures at which attack will occur ;
(4) the ability to develop in the lower
levels of soil and to withstand appreci-
able concentrations of carbon dioxide.
(Sec. 15.)
Although one strain of a fungus may
be present in a field without causing
disease, the introduction of another
strain of the same species may produce
an epidemic. Sometimes the introduc-
tion of an organism may even increase
the loss produced by a different one al-
ready present. Prompt severe losses are
usually sustained when infested stock is
planted, and clean soil may be perman-
ently infested, or the inoculum potential
of it may be increased. One of the most
dangerous features of transmission of
organisms with seed or vegetative parts
is that the constant association of the
virulent strains of a pathogen and the
host is thus assured. A second serious
factor is that many soil organisms will
persist for many years in a soil, once
introduced and established there. These
facts all emphasize the importance of
6 1
eliminating disease organisms in the
nursery, rather than merely suppressing
or fighting them. (Sec. 15.)
Don't fight 'em, eliminate 'em
Among the many advantages of free-
dom from disease in nursery crops are
the following: It is an aid to easier, more
certain, and less expensive crop produc-
tion. While growers can eventually learn
to live with a disease, they would almost
always be better off without it, because
of the enlarged growth potentialities for
the host. Thus, V erticillium wilt of
chrysanthemum can be controlled by
using resistant varieties, but more, and
in some cases better, varieties are avail-
able if this restriction is absent. Simi-
larly, losses from Phytophthora root rot
of heather can be reduced by minimal
watering, but plant growth is retarded
and more skill is required in watering
than when the disease is absent. (Sec. 3.)
The degree of financial benefit from
disease control is relative to the cultural
proficiency of the grower; the greater
the return per plant, the greater will be
the profit if disease in it is prevented.
Buying or growing pathogen-free nurs-
ery stock frequently is cheaper than
fighting the disease.
The danger of national panics in the
nursery industry, such as those concern-
ing rose mosaic in 1929-1932 and chrys-
anthemum virus stunt in 1947-1950,
would be considerably reduced if patho-
gen-free stock were generally used.
All nursery practices
must mesh
Disease in the nursery should never
be viewed as an isolated phenomenon,
unrelated to other phases of growing.
Actually it is one of a series of interre-
lated problems which must be solved
simultaneously rather than piecemeal,
for maximum effectiveness and perman-
ence. A case in point is the perennial
dilemma of southern California nursery-
men, who lose their seedlings from sa-
linity if they water lightly, and from
damping-off if they water heavily. To
successfully mechanize such a nursery
and introduce mechanical watering, the
soil pathogens must be eliminated, so
that the salinity may be held down by
copious watering, without aggravating
damping-off. Again, when soil is
steamed, the frequency and quantity of
watering must be modified because of
altered water retention. (Sees. 2 and 3.)
A disease-control program must either
fit into the current cultural methods, or
these must be modified before it can be
adopted. Often both develop together.
For example, the control of carnation
diseases has developed along with sweep-
ing changes in methods of growing: (1)
year-round glasshouse culture; (2) di-
rect benching of cuttings; (3) the single
pinch; (4) continuous forcing; (5) use
of cuttings from the new disease-free
seedlings.
These situations illustrate the basic
unity in proper nursery production pro-
cedures. If an advance is made in dis-
ease control, its successful adoption
necessitates changes in other practices,
and its benefits may project into other
aspects of nursery culture.
Salinity
Small amounts of various salts are
necessary to plant development, but ex-
cessive concentrations cause injury or
death, just as small amounts of table salt
are necessary to man but large amounts
may aggravate high blood pressure and
very large amounts may kill.
Plant injury varies
Plant susceptibility to an excess of
water-soluble salts varies widely from
almost no injury (carnation, stock; fig
3) to severe injury (plants with soft large
leaves, such as begonia and fern; figs.
54 and 55). Salinity may produce sev-
eral types of effects:
[7]
Fig. 3. Salinity injury to leaves of three ornamentals. A, Maranta leuconeura, showing leaf
with burned tip at left, normal at right. B, Apex of leaves of Cordyline terminalis, showing tip-
burn at left, normal at right. C, Leaves of stock, Matthiola incana, showing minor tipburn of old
leaf at left, and more serious injury of young leaf at right. Such injury to stock is important
mainly because it is readily infected by the Botrytis gray mold.
l.No apparent symptoms at moderate
concentrations, reduced growth at higher
levels (carnation I ;
2. Leaf burn, usually at margins I azalea I
or tips (cymbidium, Maranta, Cordy-
line; fig. 3), which makes the plant un-
sightly and weakens it;
3. Root corrosion and killing (azalea,
gardenia; fig. 56) which may, depend-
ing on severity of injury, cause chlorosis
[8]
of the leaves or wilting and collapse of
the plant;
4. Little or no germination of seed;
5. Prompt wilting, desiccation, and
death after transplanting seedlings into
saline soil;
6. Localized injury to leaves from salts
accumulatively deposited on the surface
by irrigation water (begonia) or from
contact with a salt-saturated flower pot
( Saintpaulia) .
The weakening of the plant renders
it more susceptible to attack by organ-
isms; thus seedlings may be made more
susceptible to damping-off, and stock
leaves with tipburn become susceptible
to Botrytis infection. (Sec. 4.)
Sources of salinity
Salts may accumulate from those in-
troduced into soil with: (1) irrigation
water (fig. 38), which at times is quite
saline; (2) application of fertilizers (fig.
40) in excessive amounts or of types
which leave substantial unused residues
in the soil; (3) use of manure or leaf
mold (fig. 42) gathered in places where
they have accumulated large amounts of
salt, a condition common in southern
California. (Sec. 4.)
Salts added in any of these ways may:
(1) be flushed on down by subsequent
large applications of water, and thus
leached beyond the root zone or out of
the container; (2) be absorbed by plants
and either used in their metabolism, or
accumulate and finally reach a toxic level
(as in leaf-margin or tipburn) ; (3) ac-
cumulate in the soil, being washed down
a few inches with each irrigation, only to
be carried back to the surface with the
water and deposited there as a residue
when it evaporates. It is necessary to
apply more water than is used by the
plants and evaporated from the soil sur-
face, in order to prevent the accumula-
tion of salts. The greater the salinity of
the water, the greater must this excess
be. Repeated light sprinkling leads to
trouble unless an occasional heavy leach-
ing irrigation is practiced. (Sec. 4.)
The salts may accumulate in a clay
pot in the same way, exposing the roots,
which are most plentiful next to it, to a
high concentration of salts. (Sees. 4 and
12.)
Because the concentration of salts in
soil water increases as the soil dries out,
plant injury is aggravated by either
growing plants "on the dry side" or
watering only when the soil is dry. A
consistently moist soil will give least in-
jury. (Sec. 4.)
Measuring salinity
When salinity is suspected, because of
plant injury or the type of culture, it may
be tested for by measuring the elec-
trical conductance of a saturated soil
extract with an inexpensive simple in-
strument, the Solubridge. The salt con-
tent of the water supply should be
determined, as well as that of the soil,
peat, leaf mold, manure, and so on, be-
fore they are mixed for use. This elimi-
nation of a source of potential trouble,
rather than waiting for it to develop, is
as necessary for mechanized nursery
operation as is the establishment of qual-
ity tolerances for parts used in an auto-
mobile assembly line. (Sec. 4.)
Toxicity
Use of the U. C. system of soil mixes
and nutrients has eliminated the toxic
effect from steaming or chemically treat-
ing soil. Because of this simple solution,
the problem seems to be unnecessarily
causing concern. Plants grown in con-
ventional treated soil mixes may develop
injury (stunting, dropping of leaves,
root corrosion, death ) from toxins.
These materials, which may be tempo-
rary or persist for months, result from
the formation or release of various chem-
ical materials (such as ammonium, or-
ganic matter, manganese, soluble salts).
Soil mixtures high in readily decom-
[9]
posable organic matter (manure, leaf
mold, compost) are most likely to give
injury from such treatment. Growers
who do not use mixes of the U. C. type
may reduce injury by leaching or aging
the treated soil before use, application
of gypsum in some cases, or by plant-
ing immediately after treatment. (Sec.
6.)
Injury may also result from a persist-
ent residue of the chemical used in soil
treatment (for example, on carnations
planted in soil treated with methyl
bromide). This is a different problem,
and may be prevented by using a dif-
ferent chemical, by altering the condi-
tions of its use, or by aging of soil after
treatment. (Sec. 11.)
THE ANSWERS
Disease control in the nursery is most
effective when preventive treatment aims
at eliminating the causal organisms from
the soil, from the seeds, cuttings, or other
planting material, and from the bits of
soil on tools, flats, hoses, and other equip-
ment, or in places where it may be
readily splashed by water (fig. 4). This
approach demands that preventive meas-
ures be planned in advance, rather than
waiting until trouble arises. (Sec. 3.)
The U.C. System of Soil Mixes
and Nutrients
One of the commonest erroneous ideas
in nursery practice is that a special soil
is required for each type of plant. Actu-
ally, most plants of necessity had to have
a wide tolerance of different soils in
order to survive. The basic fact that
many kinds of plants can be successfully
grown in a single soil mix, or in slight
modifications of it, was demonstrated by
the John Innes Horticultural Institution
in 1934-1939. This was an important
contribution to nursery practice, and the
J. I. mixes have been widely adopted in
recognition of this fact. They fail, how-
ever, to eliminate several serious inher-
ent disadvantages common also to
conventional soil mixes. The U. C.-type
soil mixes have corrected these objec-
tions. (Sec. 6.)
Advantages of the U. C.-type
soil mixes
The soil serves four principal func-
tions for plants: (1) it provides me-
chanical anchorage and support; (2) it
stores and makes available a supply of
water; (3) it stores and regularly sup-
plies mineral salts essential to the plant;
(4) it provides aeration for the roots.
These functions are well served by the
U. C. soil mixes. (Sec. 6.)
Certain advantages over the multi-
plicity of mixes are also provided by
the U. C.-type mixes:
1. They may be heat- or chemically
treated without producing injurious
toxic residues.
2. The variability from the use of leaf
mold, animal manure, turf, and
composts, as well as from differences
in the degree of their decomposi-
tion, is reduced, and more uniform
results are possible.
3. The salinity problem is reduced by
eliminating some of its common
sources and by providing a medium
that may be readily and effectively
leached.
4. Labor requirement is reduced.
5. The space utilized for compost piles
and storage of raw materials and
Fig. 4. Diagram of nursery soil problems considered in this manual, showing their sources and
answers. The numbered boxes on the source lines indicate the appropriate preventive measures,
named at the right.
I 10]
SOIL
P
R O
6
L
EMS
\ D
T
s /
\ 1
O
A /
\ s
X
L /
\ E
1
1 /
\ A
\ s
c
1
N /
1 /
\ E
T
T /
V s
Y
Y /
1
/
s
o
u
R
c
E
S
10
Fertilizer
Organic Matter —
Planting Stock
Containers
Recontamination
ANSWERS
1. U. C. Type Soil Mix
2. Good drainage
3. Moist soil and air
4. Leaching
5. Treating soil
6. Good water
7. Frequent light fertilizing
8. Clean planting stock
9. Treating container
10. Sanitation
[in
various mixes is saved, an import-
ant item where land is expensive.
6. Loss of volume from shrinkage during
composting of organic matter is
avoided.
7. Odors and flies from the compost piles,
likely to prove restrictive in resi-
dential areas, are eliminated.
8. The problem of the scarcity of leaf
mold, animal manure, and turf is
avoided. (Sec. 6.)
Physical components
The physical base of the U. C.-type
mix consists of an inorganic material
(fine sand, perlite, vermiculite) and an
organic fraction (sphagnum peat moss,
rice hulls, sawdust, shavings, bark). The
two components presently suggested for
use in California nurseries are fine sand
(particle size ranging from 0.5 to 0.05
mm) and sphagnum peat moss. These
components satisfy the greatest number
of desirable features (fig. 65) :
1. They are readily available in uniform
grade.
2. They are chemically uniform and
relatively inert.
3. They are not broken down by steam
or chemical treatments used to free
them of disease organisms.
4. They are easily made into a uniform
mix.
5. They provide good aeration and wa-
ter drainage.
6. The peat retains mineral nutrients
against leaching, although the fine
sand is less effective in this.
7. Their fertility is low, furnishing a
known low starting point for add-
ing nutrients.
8. They are relatively inexpensive.
(). When mixed they have good water
retention.
10. They arc light in weight.
11. They have proved adequate in micro-
nutrients, but should instances of
deficiency arise the elements can
easily be added.
12. They have negligible shrinkage in
storage and use.
Characteristics 1 through 4 are essen-
tial, and their deficiency cannot be made
up by adding or substituting other mate-
rials, as can features 5 through 12. This
fine-sand— peat mixture has most of the
good features of clay soils without their
disadvantages. (Sec. 6.)
The sand ingredient may have 12 to
15 per cent (preferably less) coarse
sand, must not have more than 15 per
cent (preferably less) clay or silt, or
both, and should have 70 to 85 per
cent or more of fine sand. A method is
available for nurserymen to determine
particle size of soil samples. Five dif-
ferent proportions of sand to peat are
suggested for different purposes:
Mix A. 4:0, sometimes used for certain
crops and bench stocks;
Mix B. 3:1, the most commonly used
ratio, for bedding plants and general
nursery planting;
Mix C. 2:2, for plants grown in pots or
benches;
Mix D. 1:3, for pot plants that are large
in relation to their containers, and
for cymbidiums;
Mix E. 0:4, for growing azaleas and
similar acid plants, sometimes
mixed with wood shavings. (Sec. 5.)
Chemical components
These U. C. mixes are purposely low in
nutrients, so that mineral elements may
be added to this known base with pre-
dictable results. Sometimes fertilizers
are omitted from the mix and applied
in solution after planting. Usually, how-
ever, they are added, at least in part, at
the time of mixing the soil. Phosphorus,
because it is applied as a slowly soluble
12 |
NOTE:
Urea and urea-formaldehyde fertilizers
may contain biuret, a by-product toxic
to many plants. Unless labeled biuret-
free, these materials should be used only
after thorough testing on each crop.
superphosphate, does not contribute ap-
preciably to the salinity problem while
supplying crop needs for this element.
Potassium is presently supplied as water-
soluble potassium nitrate or, less com-
monly, as potassium sulfate or potassium
chloride, and thus contributes to the
salinity problem. Calcium and magne-
sium are presently supplied as dolomite
lime in the soil mix. This does not con-
tribute appreciably to the salinity prob-
lem, while neutralizing the acidity of the
peat moss and supplying these necessary
elements. (Sec. 5.)
Nitrogen is generally supplied in the
organic form (hoof and horn meal, urea-
formaldehyde resin, blood meal, cotton-
seed meal, castor-bean pomace), but
sometimes as inorganic nitrogen (po-
tassium or calcium nitrate), or both.
(Sec. 5.)
Nitrogen availability
The organic nitrogen, which is un-
available to the plants, is converted to
ammonium (available to plants) by bac-
teria and fungi that are quite resistant
to soil steaming or chemical treatment;
the ammonium is changed to nitrate
(available to plants) by nitrifying bac-
teria intolerant of most of these treat-
ments. The latter step is adversely
affected by an acid medium and low soil
temperature, and therefore ammonium
tends to accumulate under these condi-
tions. Also, bacteria tend to be sparse in
fine sand obtained at a depth of a foot
or more (as much of it is in California) ,
and in this way such material resembles
treated soil. (Sees. 6, 7, and 14.)
Under average conditions treated soil
containing organic nitrogen does not, for
a variable period (about 1 week), pro-
vide nitrogen in a form available to
plants, then presents it in the form of
ammonium for another period (about 2
weeks), and thereafter as both am-
monium and nitrate. Seedlings grown in
a newly treated soil containing only
organic nitrogen are often deficient in
nitrogen, a situation readily corrected by
watering with a calcium nitrate starter
solution at time of planting. (Sec. 7.)
Nursery crops differ in their response
to ammonium. Many types of crops (for
example, foliage plants) utilize the am-
monium nitrogen without ill effect, and
these are successfully grown with the
organic source. Other plants (for ex-
ample, sweet alyssum, clarkia, and car-
nation) show injuries varying from
leaf burn and root injury to death, when
supplied ammonium nitrogen. Petunia
and snapdragon seedlings may show ex-
cessively soft growth and iron chlorosis.
This injury is worst to plants in the
seedling stage. In such cases the organic
nitrogen should be eliminated or reduced
in amount, and nitrate fertilizer should
be supplied. (Sees. 5, 7, and 14.)
The quantity of organic nitrogen sup-
plied varies with the size of the plant in
relation to the volume of soil in the con-
tainer, and is greatest for large plants in
small containers.
It may be possible to inoculate treated
soil with nitrifying bacteria in order to
lessen the ammonium increase, but the
effect may not be evident for 10 to 20
days. If this is done, nitrifiers should be
introduced without ammonifiers, or the
situation may be worsened. (Sees. 5, 7,
and 14.)
Because the breakdown of organic
nitrogen occurs in a stored U. C.-type
mix, the high content of water-soluble
forms of nitrogen may cause plant injury
if the soil is held for several weeks be-
tween mixing and planting. If such
storage is planned, one of the fertilizer
variants should be used that does not
[13]
include the organic form of nitrogen;
this form should be applied as a top
dressing after planting. (Sees. 5, 7, and
14.)
Selecting nitrogen fertilizers
The organic forms are slowly available
and, therefore, present a continuous low
supply rather than the varying quantities
resulting from occasional applications of
inorganic forms. In descending order for
rate of conversion and ascending order
for nitrogen content, the organic nitro-
gens tested were: castor pomace; fish
meal; cottonseed meal; blood meal and
hoof and horn meal; urea-formaldehyde
resins. The urea-formaldehyde resins
are apparently hydrolyzed by steaming
and may therefore give rapid ammonium
build-up; these materials must be free of
biuret to be safe for use on nursery
plants. Hoof and horn meal and blood
meal are presently considered best for
the mix. (Sees. 5 and 7.)
Surface dressings of these organic ma-
terials do not lead to injury from am-
monium, because of the slow rate of
penetration of ammonium through soil;
it is normally converted to nitrate before
reaching the root zone. (Sees. 5 and 7.)
The nitrate forms are immediately
available and eliminate the hazard of
ammonium accumulation. They are
therefore useful (1) in mixes when nitri-
fying bacteria are absent (sees. 7 and
14) ; (2) in starter solutions for seed-
lings in treated mixes containing organic
nitrogen (Sec. 7) ; (3) when soil mixes
are to be stored (Sec. 5).
Fertilizer application
Where plants are to be carried in
containers or benches for an extended
period of time, it becomes necessary to
replace fertilizers which are lost through
plant uptake and leaching. Dry fertilizer
may be broadcast over the surface and
watered in, or liquids may be applied in
the irrigation water itself. (Sec. 5.)
I sually dry fertilizers should include
an organic source of nitrogen, in order
to prolong the effective period and reduce
the salinity hazard. There is no problem
with ammonium from such application,
even though it may be formed. Am-
monium does not move readily down
past the surface layer of soil until broken
down by microorganisms to nitrate. The
other components of the fertilizer should
be superphosphate and potassium sulfate.
(Sees. 5 and 7.)
Liquid fertilizers may contain any one
of several nitrogen sources. Ammonium
nitrate or urea is commonly used, as
they can readily be mixed with any other
ingredients. Calcium nitrate should be
used where an all-nitrate form is desired,
but this source of nitrogen should not be
mixed with sulfates or phosphates in con-
centrates because it forms insoluble salts
of calcium phosphate and calcium sul-
fate. Phosphate is easily supplied as
mono-ammonium phosphate, and potas-
sium as potassium chloride. Other mate-
rials can be used, and examples of rates
and formulas are outlined. (Sees. 5 and
7.)
Preventing Salinity Injury
Excessive concentrations of salts may
be avoided through detection of accumu-
lation at an early stage by measuring the
electrical conductance of soil samples,
and taking active preventive measures.
Once the plant is crippled by root injury
or leaf burning, rehabilitation is slow,
and seldom economic for a nursery
crop. Preventive measures include:
1. Use excess water over that required
for plant absorption and evapora-
tion from the soil, assuring drainage
from the root zone with each water-
ing.
2. Use the best possible quality of water
(low salinity; conductance less than
1.0, or 650 ppm), and avoid saline
waters, particularly on sensitive
plants.
3. Leach with a considerable excess of
water whenever salts reach a dan-
I 14]
gerous level (conductance of satura-
tion extract about 3.0, or 1,950 ppm
for most crops) ; the higher the
salinity of the water or soil the
greater the quantity of water that
must be used.
4. Use deionized water for some of the
more expensive crops.
5. Expose soil and plants to rainfall
(salt-free) when feasible.
6. Maintain excellent drainage (unob-
structed drainage holes in pots and
cans; open cracks in bottoms of
benches; avoid hardpan soils below
ground beds; install drain tiles
when needed; use porous soil) so
that salts may be readily flushed
from the soil.
7. Use a U. C.-type soil mix with the
organic matter in small pieces;
avoid loam (even if Krillium-
treated) , as it does not leach readily.
8. Avoid soil, manure, leaf mold, black
peat, and kinds of sewage sludge
high in soluble salts or, if they must
be used, leach them heavily before-
hand.
9. Apply fertilizer in frequent small,
rather than in a few heavy, applica-
tions.
10. Avoid mixed fertilizers that include
minerals not needed at all or not in
amounts supplied.
11. Grow plants with the greatest shade
and humidity compatible with good
culture of the crop, so as to decrease
salt concentration and injury.
12. Keep soil as uniformly moist as is
compatible with good culture of the
crop, avoiding alternating wet and
dry soil conditions.
13. Add organic matter to the soil to
stabilize moisture content and reduce
injury.
14. Soak old clay pots before re-use to
remove accumulated salts.
15. Avoid overhead sprinkling of plants
(begonia) subject to leaf burn from
salt left from evaporated water
drops.
The U. C. system of soil mixes is com-
pletely compatible with these measures,
either incorporating them or making it
possible to follow the procedures. (Sec.
4.)
Treatment of Soil by Heat
Heat treatment is used to free soil of
organisms which cause plant disease, as
well as of weed seeds and insects. Steam
treatment of soil remains the best method
of disinfestation for all fungi, bacteria,
nematodes, weed seed, and insects. (Sees.
8 and 9.)
Temperature requirements
and soil preparation
Heat treatments in which a temperature
of 180° F is maintained for 30 minutes
are adequate; with many methods, how-
ever, the process cannot be stopped short
of 212°. With the U. C. system of soil
mixes there is no residual toxicity from
heating in either case. The soil should be
in good planting tilth, well mixed, free
of clods, and with sufficient moisture so
that after being squeezed in the hand it
will crumble easily. For economical
treatment, the soil should not be soggy,
because five times more heat is required
to heat water than soil. After cooling, the
soil is in good planting condition, with-
out excessive moisture. (Sec. 8.)
Methods
Treatments are preferably applied
after the soil is mixed and placed in tlie
containers, since this method reduces the
recontamination hazard from handling.
Some of the bulk methods of soil treat-
ment are, however, satisfactory if mech-
anized to minimize the handling. (Sees.
8, 9, and 10.)
Steam is most economically used in
the free-flowing form. When steam is
released into soil under pressure it
[15]
immediately reverts to 212° F and the
nonpressure (relative to atmospheric
pressure) condition; therefore, there is
little advantage in using it. Since super-
heated steam provides a little more heat
per pound and contains somewhat less
entrained water, there are some slight
advantages in using it, although equip-
ment of this type is not commonly
available in this country. (Sees. 8 and 9. )
The quantity of steam needed to raise
the soil temperature to 212° F varies with
many factors, but a generally accepted
working average is 6.5 pounds per cubic
foot of soil, or 42 B.t.u. per cubic foot
per degree of rise. The amount of soil
that can be steamed in a given time using
boilers of various sizes is given in table
14. One of the advantages of steam for
soil treatment is that it may be used near
living plants without injuring them; it
is neither toxic nor unpleasant to work-
men. (Sees. 8 and 9.)
Equipment
Many kinds of equipment have been
designed for steaming soil, and these
have been grouped in this manual into
thirty-five types. Nine of these (types 2,
4a, 4b, 5, 6, 7, 18, 19, and 29) seem well
adapted to California conditions. (Sec.
10.)
For treatment of bulk soil, stationary
or mobile steam boxes (type 4, fig. 5) or
the mobile bin (type 2, fig. 80), both
with perforated pipe grid and a sta-
tionary soil mass, are excellent. The
feature of continuous output may be
combined with the advantages of having
a stationary soil mass in the continuous-
batch modification of types 2, 4, 6, or 9
(fig. 6) . For a continuous output of bulk
soil, the rotating-screw type with injected
steam (type 29, fig. 100) is satisfactory.
For treatment of soil in containers, the
Thomas method (type 5), the vault (type
0. fig. L31), and the multipurpose tank
(type 7, fig. 85) arc recommended. The
Thomas method (type L8, fig. ()\ I and
the inverted steam pan (type 19. fin. 92 I
are the most convenient for treating soil
in benches and beds, but are not depend-
able below 8 to 9 inches in depth. If deep-
er treatment is required, the buried per-
forated pipe (type 20, fig. 93) or the
permanent buried tile (type 22, fig. 95)
may be used. (Sec. 10.)
Equipment in which a stationary soil
mass is treated raises the temperature to
212° F when steam is used, and even
higher if electric immersion heaters are
employed. When steam is used, equip-
ment with a stationary soil mass is prob-
ably best, although some with a moving
soil mass are satisfactory. When heat
from immersion units, hot plates, and
other dry sources of heat is used, it is de-
sirable that a type with a moving soil
mass be employed, since there is charring
of organic matter in types with a station-
ary soil mass. The use of hot water for
soil treatment is suitable only for propa-
gating sand. One should use table 15 to
determine the types of equipment with
the necessary features for a given instal-
lation, and then refer to the text for
details. The size of the boiler required
may be estimated from table 14. (Sees.
9 and 10.)
Natural gas is the cheapest fuel in
California. Oil and butane are more ex-
pensive but better adapted to portable
equipment. Electricity is very expensive
to use for soil treatment, but is very
convenient. (Sec. 10.)
Steam versus chemicals
Steaming soil requires about an hour,
plus another hour to cool before plant-
ing; methyl bromide is used in a 24- to
48-hour treatment, plus a 24- to 48-hour
aeration; chloropicrin is used in a 48-
to 72-hour treatment, plus a 7- to 10-day
aeration. Steam is effective against all
organisms except a few types of weed
seeds; methyl bromide is only partially
effective against Verticillium, and leaves
a residue toxic to some plants (carna-
tions; snapdragon seedlings); chloro-
picrin is generally effective against
[10]
Fig. 5. The removable-front steam box for stationary bulk soil, and for soil in containers
(Sec. 10, type 4b). See also fig. 82.
Fig. 6. Pressure autoclave for treatment of flats of soil (Sec. 10, type 9). The flats are
placed in a special rack and rolled into the unit for steaming. (Photo courtesy of American
Plant Growers, Lomita, California.) See also fig. 86.
[17]
organisms except those in root masses,
and leaves no toxic residue unless im-
properly used. The cost of treatment
with steam (including cost of boiler) is
less than 2.0 cents per cubic foot; for
methyl bromide it is about 2.9 to 3.2
cents, and for chloropicrin about 1.9 to
3.0 cents; labor is excluded in these cal-
culations. (Sec. 8.)
Regardless of the method of treatment,
if clean soil is dumped in bulk piles on
the floor, the surface should previously
have been wet down with a formaldehyde
solution (1 gal. to 18 gal. water). (Sees.
8 and 11.)
Treatment of Soil
by Chemicals
When a source of steam is not avail-
able, or when an area of field soil is to
be treated, chemical applications are
often used. Fungi are harder to kill in
the soil with chemicals than are nema-
todes, insects, or weed seeds. When soil
fungi are involved, the chemical and
dosage must be adequate to kill them;
this dosage will usually also kill the
nematodes, insects, and weed seed.
Nematocides (DD, EDB) often have
little fungicidal value, and insecticides,
weed killers, and soil conditioners are
also largely ineffective against fungi or
bacteria. (Sec. 11.)
Methyl bromide
Nursery soil in containers is commonly
treated with gaseous methyl bromide in
California. The stacked flats, pots, cans,
or small piles of soil are covered with a
tight plastic tarpaulin, and the gas re-
leased under it from pressurized cans or
cylinders (figs. 106 and 107) at the rate
of 4 pounds per 100 cubic feet of en-
rlosrd space If tin1 temperatures are
low, the gas is passed through a copper
pipe immersed in hot water to volatilize
any Liquid methyl bromide. The soil is
left covered for 21 to 18 hours, and
aerated for 24 to 48 hours before use.
This is an effective and commonly used
treatment, but should not be applied to
soil to be used for carnations or snap-
dragon seedlings because of residual
toxicity, or for chrysanthemums because
of its ineffectiveness against Verticillium.
(Sec. 11.)
Chloropicrin
Chloropicrin is more generally useful
and cheaper, but because it is less con-
venient and takes longer to aerate, it is
less commonly used in California. It has
not been commonly used for treating
stacked containers of soil. On beds it is
injected 6 inches deep with special
equipment (fig. 105), at the rate of 2 to
3 cc per 10 inches square of soil, and is
confined either by wetting the top inch
of soil or by covering it with a plastic
tarp. Bulk soil may be treated in bins,
drums, or any gasproof receptacle at the
rate of 3 to 5 cc per cubic foot. Treat-
ments with chloropicrin are for 48 to 72
hours, plus a 7- to 10-day aeration before
planting. (Sec. 11.)
Vapam
This new water-soluble material is be-
coming widely used, especially for
ground beds and field soil. It is applied
at 1 to 2 quarts per 100 square feet,
either on the surface with irrigation
water or injected into the soil. Soil may
be cultivated after 7, planted after 14
days. (Sec. 11.)
Nematocides
DD is used for nematode control in the
field at 200 to 400 pounds per acre, and
the soil may be planted after 1 to 2
weeks. Ethylene dibromide (EDB) is
used against nematodes at the rate of 3
to (> gallons per acre, and soil may be
pi an led after 2 to 3 weeks. Neither of
these last two materials is recommended
against fungi or bacteria. (Sec. 11.)
[18]
Spot treatments
Spot treatment of limited areas of
fungus infection is desirable to prevent
spread to other plants, but it should
never be made the complete control pro-
gram, as it is in some nurseries. Such
spot treatments are not eradicative and
merely aim to make the best of a bad
situation. The disease suppression af-
forded is temporary and in many cases
not very satisfactory. Materials used in-
clude ferbam, thiram, and captan (1
tbsp. per gal. of water, per 8 to 16 sq.
ft.), Semesan (1 tbsp. per gal. of water,
per 24 sq. ft.), nabam (1 fl. oz. per 4 to
8 gal. of water, per 64 sq. ft.), and Ter-
raclor (1 oz. of 75 per cent wettable
powder per 42 to 63 sq. ft.). In treat-
ment of flats the whole surface should be
drenched; in the field the removal of dis-
eased plants may be desirable and the
drench should be applied to an area 1 to
2 feet beyond the margin of disease.
(Sec. 11.)
Treatment of Containers
Flats, pots, cans, benches, and pallets
should be treated with heat or chemicals
before being re-used. Preferably the raw
soil mix is placed in the container and
both are treated together, but treating the
containers and soil separately is often
practiced.
Heat
If steam is used for treatment of con-
tainers, a temperature of at least 180° F
should be maintained for 30 minutes, the
same as for soil. With clay pots perhaps
the best method is to soak thern in water
of 180°-212° for at least 30 minutes,
since this removes the accumulated salts
and kills pathogens and algae in the sur-
face slime as well. The prevalent practice
of going over a bench with a blow torch
is without disinfesting value; heat of this
type is so concentrated as to char the
wood, but so short that heat does not
penetrate. Steam provides the steady
penetrating heat needed for this work.
(Sec. 12.)
Chemicals
Chemicals may be effectively used for
treatment of containers. Methyl bromide
may be used for fumigation by treating
stacked flats exactly as for soil above;
they should be aerated for 1 day before
use. Formaldehyde ( 1 gal. of 37 per cent
commercial formaldehyde per 18 gal.
water) may be used for dipping con-
tainers or may be sprayed on them, using
a coarse nozzle. In either case they should
be stacked wet and covered with a tar-
paulin for 24 hours and then should be
aerated for at least 4 to 5 days, being
kept wet to prevent the formation of the
slowly volatilizing paraformaldehyde.
Tools may be dipped for a few minutes
in a crock of this solution, rinsed with
water, and used at once. Copper naphthe-
nate applied to flats affords a self-disin-
festing surface residue for at least a
year; there is no carryover of damping-
off organisms on containers treated in
this way. It is least expensive when pur-
chased in the 8 per cent concentrate, and
diluted (1 gal. to 3 gal. of Stoddard
solvent per 800 to 1,600 sq. ft.) for
dipping or painting on wood containers.
It is an excellent wood preservative. Such
containers may be steamed, but need not
be if they are freed of lumps of soil and
roots. Since there is some root injury, the
material should not be used on seed flats
or benches where plants are set less than
2 to 3 inches from the sides. It is excel-
lent for treated benches, shelves, and
timbers on which containers are set, and
may be used for disinfesting an empty
bench in a house full of plants, if the
vents are kept open for a day. (Sec. 12.)
Development and Maintenance of
Healthy Planting Stock
For the preceding soil treatments to be
really effective it is necessary that healthy
stock be planted in such soil, because
[19]
diseased plants are centers of infection
for healthy ones, this spread of disease
often being more rapid in treated than in
untreated soil. This unfortunate effect
from treating soil is actually more of a
mental than a practical obstacle at pres-
ent, and it may be possible eventually to
eliminate it through the use of antago-
nistic or retardant organisms. (Sec. 14.)
Pathogens introduced into a planting
are more dangerous if they infest the soil
than if they do not, and the longer they
are able to persist in it the greater the
danger. Most of the pathogens with
which we are concerned in this publica-
tion more or less permanently infest the
soil. (Sec. 13.)
Obtaining clean stock
Clean stock or seed may be initially ob-
tained in the following ways (Sec. 13.) :
1. From a specialist propagator who
has maintained it. It is as much a
duty in the nursery world to report
to the propagator any stock that
carries disease as it is to vote in
the political world, and for much
the same reason.
2. From a few healthy plants that may
be available.
3. By using practices which enable a
few plants to grow away from the
pathogen. Tip cuttings produced
12 inches or more above the soil
may be taken from plants grown
in areas as nearly free of disease
microorganisms as possible, and
without overhead sprinkling. Cane-
producing and trailing plants may
be trained up off the ground to
achieve this. In exceptional cases
aseptic culturing of tiny apical
growing points may be used to pro-
vide a nucleus of healthy stock.
1. By using cultured-cutting techniques
(fig. 109) to obtain a nucleus of
disease-free plants. This has been
done commercially for chrysanthe-
mums, carnations, roses, and gera-
niums. It will not eliminate virus
infections, however. The technique
involves culturing from the base of
each cutting; those that are found
to be clean form the nucleus for
further propagation. This involved
technique has been most effectively
used by specialist propagators, less
so by growers.
5. By heat treatment of planting stock.
This has been applied to a wide
range of ornamentals including
foliage plants (figs. 112 and 114),
succulents (fig. Ill), seeds, corms,
bulbs, plants, and cane. It is based
on the greater heat sensitivity of
the pathogen than the host, and
each treatment is therefore spe-
cific. Methods must be evolved for
each parasite-host combination
and must be carefully followed.
The central idea is to obtain a
nucleus of clean stock, and to do
this even high mortality from the
heat treatment is justified. Actually,
however, there is very satisfactory
survival in most cases. The cleanest
most vigorous stocks or seeds
available should be used, and they
should be in a state to withstand
treatment or be conditioned for it.
The key to success in many cases
lies in using heat-resistant plant
material. Temperatures range from
115° to 131° F for 10 to 40 min-
utes for different plants; details
are given in Section 13.
6. By chemical treatment. This has
limited use in eradicating an or-
ganism in host tissue (calla rhi-
zomes treated with formaldehyde,
mercuric chloride, or New Im-
proved Ceresan ; chrysanthemum
sprayed with parathion against
foliar nematode), for purposes
here considered. It is primarily
useful for protective purposes, to
20
prevent an organism from invad-
ing the coated tissue, especially
with seeds.
7. By sanitary practices. Though rarely
capable of providing clean stock,
these will do so in the cases of
camellia and azalea flower blight
through elimination of carryover
sclerotia.
8. By aging of seed. This sometimes
frees the seed of an organism;
celery seed 3 years or more old is
thus freed of Septoria late blight.
9. By prolonged roguing of diseased
plants from a stock. This will
gradually free it of a disease that
does not spread in the field (for
example, rose yellow mosaic in a
mother block).
10. By growing plants from true seed
rather than from vegetative parts.
This is particularly effective
against viruses (ranunculus, free-
sia, anemone, yellow calla).
11. By selecting areas for producing seed
or propagative material where the
climate exerts a naturally restric-
tive effect on the organism in ques-
tion. This will help in obtaining
pathogen-free stock. (Sec. 13.)
Maintaining clean stock
The maintenance of the healthy status
of a stock must involve certain safe-
guards.
1. New stock brought in should be iso-
lated in an introduction "pest
house" to determine its state of
health before it is planted in clean
production houses.
2. Propagation operations should be iso-
lated from all possible sources of in-
fection; they should not be con-
ducted in weedy areas or known dis-
ease centers.
3. The production and merchandising of
plants on the one hand, and the
maintenance of the basic stock for
future propagation on the other,
must be handled as independent and
isolated activities (fig. 115). This
mother-block principle is effective
because it is easier to care for and
protect a small block than the large
production areas. It is a practice
worthy of far greater adoption by
the nursery industry.
4. The sanitary procedures outlined in
sections 3 and 14 should be care-
fully followed. (Sec. 13.)
Preventing Recontamination
The natural soil contains a vast popu-
lation of roots of higher plants, algae,
fungi, bacteria, actinomycetes, insects,
nematodes, protozoa, and other organ-
isms. These exist in a state of dynamic
equilibrium or fluctuating balance, com-
peting with each other for food and
space. One may become temporarily
dominant due to some change (for ex-
ample, a favorable food, temperature,
moisture), but soon is submerged by the
parasitic, competitive, or antibiotic ac-
tivities of other organisms. (Sec. 14.)
Parasitic fungi and bacteria generally
have been weakened for such competi-
tion by the very specialization required
for their attack on higher plants, and are
unable long to withstand the survival
pressure in the soil. The more highly de-
veloped the parasitic activity, and the
more able the organism is to attack a
vigorously growing plant, the less able
it usually is to survive under natural
competition. When the host is present,
competition is evaded by utilizing the
specialized food source (living plant)
which the saprophytic forms cannot at-
tack. Specialized parasites, such as the
geranium leaf spot and stem rot bac-
terium and the fungus that causes flower
blight of azalea, survive for a relatively
short time in natural soil free of the
hosts. Generalized parasites that only in-
fect weakened plants (the bacterium that
causes soft rot of many hosts, and many
[21]
of the water molds) remain as part
of the soil flora, even without the pres-
ence of a host. (Sec. 14.)
Effect of eliminating soil
microorganisms
The first organisms to return after an
eradicatory soil treatment obviously will
luxuriate. If a crop is planted in treated
soil it will generally grow better than in
an untreated soil, because many soil
microorganisms are largely crop-antago-
nistic, even though they may not produce
disease. Similarly, the first microorgan-
ism which returns develops abundantly,
sometimes visibly, in treated soil. If this
organism is capable of causing disease, a
severe outbreak may occur. This is the re-
contamination problem; the risk is
highest in the first week, before relatively
harmless air-borne bacteria and molds
reinfest the soil. (Sees. 3 and 14.)
If a soil fungicide is used at lower or
considerably higher than recommended
rates, or if one is used that is effective
against most organisms but not some
given pathogen (for example, methyl
bromide against Verticillium) , the same
effect may be attained. Therefore, one
should use recommended dosages of a
soil fungicide known to be adequate for
the job. (Sees. 11 and 14.)
The common potential sources of re-
contamination in the nursery have been
outlined above ("The Problems — Dis-
eases") and in Section 3. The preventive
procedures are summarized below in "A
Nursery Sanitation Code."
A Nursery Sanitation Code3
Treat all soil used with either steam or
chemicals. The chance of recontamination
will be reduced if all soil in a given glass-
house area is treated. (Sees. 8 and 11.)
Segregate the clean treated pots and
flats in definite areas of the workroom, iso-
lated from used untreated containers. Don't
place an untreated pot or flat in a pile of
clean containers. Never store clean ones
on the ground. (Sec. 3.)
Treat floors with formaldehyde solution
before dumping treated soil on them. Pal-
lets for flats and pots should also be
treated. (Sees. 8, 11, and 12.)
Don't plant clean seed or stock in un-
treated soil. Don't transplant infested seed-
lings into treated soil. Don't place clean soil
in untreated containers. (Sec. 3.)
Either use pathogen-free stock from a
specialist propagator, or treat your own
selected material with heat or chemicals to
insure its health status. (Sec. 13.)
Use top cuttings from the cleanest plants
you have, grown on supports up off the
f Since it is impossible to foresee all possible
transgressions, only those actually encountered
in commercial production have been listed.
Specialist propagation of pathogen-free plant-
ing stock is not considered here.
ground. Don't use cuttings taken from
plants at or near soil level unless you are
certain of their freedom from disease. Don't
use root divisions unless absolutely neces-
sary. (Sees. 3 and 13.)
In taking cuttings, break them off when
possible, rather than pinching or cutting
them. If knives are used, soak one in disin-
fectant while using the other, alternating
them at frequent intervals. In mother blocks,
knives should be treated before starting
each new plant. (Sees. 3 and 13.)
Place clean planting material only on
treated surfaces of benches, flats, baskets,
etc., or on previously unused newspaper or
wrapping paper; never place it on the
ground. (Sees. 3 and 13.)
Don't dip clean planting material in
water unless absolutely necessary. Never
dip clean planting material into a tank used
previously for infested stock. Don't use
hormone solutions on cuttings of uncertain
health; dust hormone powders onto the cut
ends of stems. (Sec. 13.)
Discard seed flats with any diseased
seedlings, or if it is absolutely necessary to
use them, transplant only from spots remote
from diseased areas. (Sec. 3.)
Segregate propagation activities and
mother blocks from crop production, and
[22]
Fig. 7. A 20-gallon crock containing a solution of 1 gal. of commercial formaldehyde to 18
gal. water. Before use, tools are dipped into the solution for a few minutes and the excess
drained or rinsed off, or allowed to volatilize. Fig. 8. (Right) The nozzle of the water hose
should be kept off the ground when not in use.
isolate them from commercial areas. Main-
tain them as separate operations. (Sec. 13.)
Avoid handling treated soil unnecessarily.
Treat soil directly in the containers when-
ever possible. Don't nervously dip hands
into bench soil while conversing near by.
Don't unnecessarily feel the soil for moisture
content, or knock plants out of pots, unless
the hands are clean. (Sees. 3, 8, 1 1, and 12.)
Avoid splashing infested soil particles
into treated soil. Don't walk over treated
flats of soil, expose treated soil to blowing
dust, or kick dust into treated soil. (Sec. 3.)
Treat tools with disinfectant before using
in treated soil (fig. 7). Use clean or treated
cloth or papers to cover seed flats. (Sec. 3.)
Place flats on 2 x 4 timbers treated with
copper naphthenate or on polyethylene
sheets, for hardening plants outdoors.
Never place flats of plants directly on soil.
(Sees. 3 and 12.)
Steam benches or beds after each crop
is removed, even if it was grown in pots or
flats. If the glasshouse is free of plants,
chemical fumigation may be used. This is
sanitation insurance. (Sees. 8 and 12.)
Hang the hose nozzle on a hook on the
side of the bench when not in use (fig. 8);
never drop it on the ground. (Sec. 3.)
Wash the hands after working with any
soil or planting stock not known to be clean,
before handling clean materials. (Sec. 3.)
Use ditch or surface irrigation with slow
stream of water (no lateral flow) on plants
used for propagation material. Don't use
overhead sprinkling on mother blocks. (Sees.
3 and 13.)
Place all new planting material of un-
certain health in a special isolation ward
until you know it is healthy. Never place it
in the middle of or near clean plantings.
(Sees. 3 and 13.)
Don't underrate the danger of introduc-
ing an organism into your nursery or fields
because it "sounds" like one you already
have. Consider organisms as different-
even though they are called by the same
name— until they are proved otherwise.
(Sec. 15.)
Remember that many organisms which
cause seedling diseases also attack mature
plants, perhaps years later, reducing yield
or killing them. Don't use palliative meas-
ures (soil drenches, sphagnum cover, etc.)
against seedling diseases. (Sec. 3.)
Use clean stock in treated soil and
containers, and practice sanitation to
keep them disease-free. Don't fight
diseases, eliminate them.
[23]
The sanitation requirement is
not unreasonable
One of the principal objections by
growers to the whole program is that an
impossible degree of hospital cleanliness
is demanded. This is not the case; it
would be more accurate to say that or-
dinary household cleanliness is expected.
The housewife fully cooks pork to avoid
giving her family trichinosis, and uses
only pasteurized milk to protect them
from undulant fever; the nurseryman
treats soil to prevent infecting his plants
with nematodes and fungi. The house-
wife washes and peels fruits and vege-
tables to prevent disease; the nursery-
man should use only pathogen-free stock
for the same reason. In washing dishes
she is reducing the danger of spreading
colds among her family; in disinfesting
the flats, pots, and so on he is only taking
comparable precautions for his plants.
As she usually does not use food that has
dropped on the floor, so he should not
place clean flats of seedlings on infested
ground. It is not as fussy to avoid walk-
ing across flats of treated soil as it is to
avoid tracking mud into a clean kitchen.
It is accepted practice to sneeze or cough
into a handkerchief to prevent spreading
colds; similarly a grower will avoid
scattering infested soil in watering and
handling. One is at least as likely to
spread disease among plants by scooping
up soil from infested beds or ground in
the hose nozzle as to spread sickness by
using another's drinking glass. Growers
should use treated tools to prevent dis-
ease spread in the nursery for the same
reason that we use only our own tooth-
brush and towel. One does not visit
friends while suffering from mumps, nor
should one introduce new plants of un-
certain health into the middle of a large
planting of painstakingly acquired
healthy stock.
As modern civilization evolved, these
accepted modem health precautions were
first unknown or ignored, then scorned
as Fussy, then grudgingly adopted, and
finally accepted as standard procedures.
Even today primitive people ridicule
many of them. Nursery practice for dis-
ease control is similarly developing. At
which evolutionary level do you stand in
your attitude toward these inevitable de-
velopments?
Retardant organisms
Although much more information is
required before the use of retardant
organisms is commercially feasible, its
potentialities for nurserymen are great.
(Sec. 14.)
Rather than leaving to chance the re-
contamination organism and the time of
its introduction, it may be possible to
introduce, after soil treatment, a specific
organism. This would be selected for its
ability to inhibit the development of sub-
sequently introduced pathogens by pro-
ducing an antibiotic in place, by compet-
ing for available nutrients, or by parasit-
izing the pathogen. This controlled colon-
ization of the soil may perhaps best be ac-
complished by using a selected group of
organisms, retardant to pathogens,
including some which develop at the
various soil temperature and moisture
ranges to be encountered. At least one of
the organisms would always then be ac-
tive. Because of the delicate balance be-
tween the inhibitory action on pathogens
of the antibiotic produced, and its toxic
effect on other beneficial organisms and
on the crop itself, the more uniform,
duplicable, and controlled the soil condi-
tions are, the better the chance of success.
The adoption of the U. C. system of soil
mixes thus brings closer the possible
commercial application of this method
by stabilizing many of the conditions. A
suspension of the beneficial organisms
could be atomized over the surface of the
treated soil in flats prior to planting. The
use of antagonistic soil organisms and
the adoption of some uniform soil sys-
tem may enter general nursery practice
together, reinforcing and modifying each
other in the process. I Sec. 14.)
[24]
Rhizoctonia damping-off has been ex-
perimentally controlled in a U. C.-type
soil mix under conditions entirely com-
parable to those of a California bedding-
plant nursery. Species of Myrothecium,
Penicillium, Trichoderma, Streptomyces,
and Plicaria prevented Rhizoctonia
damping-off of pepper seedlings, even
when inoculated at the same time as the
parasite (figs. 121, 122, and 123). Under
some conditions the presence of these re-
tardant organisms was slightly injurious
to the host as well as the parasite. (Sec.
14.)
Nitrifying bacteria might be inocu-
lated into the soil at the same time as the
antagonists, perhaps reducing the time
before nitrate becomes available to the
plants. (Sec. 14.)
No success has been attained from
adding these organisms to raw soil under
natural conditions. The microbiological
flora of a given natural soil is well bal-
anced and has increased to the capacity
of nutrients and space under the given
environmental conditions. In a word, it
is biologically buffered against any or-
ganisms that are subsequently intro-
duced. Some shock is necessary to upset
this balance before effective addition of
beneficial organisms is possible. This
shock may be achieved by soil treatment,
by addition of a nutrient particularly
favorable to the organisms added but not
to others, and perhaps by modifying soil
moisture or temperature. (Sec. 14.)
Mechanization in the Nursery
The California nursery industry has
not been slow to capitalize on the adapt-
ability to mechanization of the whole
U.C. system of soil mixes and handling.
Every nursery has special features
around which mechanization must be
designed. Certain general ideas of wide
utility have been developed, however
(fig. 126). (Sec. 17.) Among these are
the ones described in the following para-
graphs.
Mixing, filling, and
treating operations
A skip-load tractor is used to transport
the soil ingredients from the storage piles
to a large concrete mixer, in which they
and a measured amount of water and
fertilizers are mixed. The mix may be
dumped directly into a mechanical flat
filler (figs. 9 and 127), can filler (fig.
10), or pot filler (fig. 135), after which
the containers are stacked on wooden
pallets. Alternately, the soil may be
dumped into a bulk soil treater and from
this into treated containers as above. The
untreated containers and soil are loaded
into a steam cooker (figs. 6 and 131) or
stacked in piles for chemical treatment
(fig. 107), the handling being done by
a fork-lift tractor. After treatment the
containers of soil may be stored for a
few days. The flats are coming to be
subdivided by insertion of smaller re-
movable containers, each holding a dozen
plants. (Sec. 17.)
Planting and transplanting
operations
Flats have been planted by machinery
when large seeds were used, but there are
some difficulties with tiny seed ( snap-
dragon, petunia). Attempts to increase
the size of small seed by pelleting have
been only partially successful because of
reduced germination. Successful equip-
ment to space-plant tiny seed may soon
be available. At present, seed is sown in
flats for later hand-transplanting; indeed
it is possible that this laborious process
may not soon be abandoned, because it
provides the opportunity to group uni-
form-sized plants together. To balance
this point, however, there is the delayed
development (10 to 20 days) resulting
from the transplanting operation. (Sees.
16 and 17.)
Plants for field use (celery, peppers,
eggplant, tomato, or plants grown for
flower-seed companies or cut-flower
growers) have been grown from me-
chanically seeded flats. When this is
[25]
:■■.;.■
Fig. 9. Equipment for filling flats with soil. Fork-lift tractor for conveying stacks of flats on
pallets to treating equipment. (Photo courtesy of American Plant Growers, Lomita, California.)
See also fig. 127.
done, the seed may be sown by a vacuum
plate and then covered with tissue paper
and sterile sand. The flats are then
watered, stacked, and placed in a germi-
nation room of high humidity and con-
stant temperature. Some growers cover
them with polyethylene sheets, or place
individual flats in bags of this material.
When the seedlings are just emerging,
the flats are moved into the glasshouse
on temporary lines of steel rolls. Such
handling requires absolute freedom from
Fig. 10. Automatic filler for 2- or 5-gal. cans which places soil in containers and forms a
central depression in which the liner is planted. (Photo courtesy of Oki Nursery, Perkins, Cali-
fornia.) See also fig. 135.
damping-off, and must be confined to
large lots of the same variety. It saves
using the glasshouse for as much as 10
days during germination, and provides
more uniform moisture conditions with
less labor than can be maintained in the
open glasshouse. Adaptations of these
methods have been made for planting
in cans and pots, and such equipment is
presently being tested by growers. (Sees.
16 and 17.)
Watering
Watering of the containers in the
glasshouse may be done mechanically
with overhead sprinklers or other meth-
ods. In some cases fertilizers have also
been applied in this way, perhaps fol-
lowed by a water rinse. The excellent
drainage and aeration of the U. C.-type
mix greatly facilitates this method of
watering, as there is slight danger of
overwatering. The freedom from disease
reduces the possibility of spread of or-
ganisms during this operation. Further-
more, it has been found that seedlings de-
velop faster (5 to 11 days for celery) in
a U. C.-type mix than in standard ma-
nure formulas. (Sees. 16 and 17.)
THE FUTURE
A unified positive system for the pro-
duction of healthy nursery stock is out-
lined in this manual. Maximum benefit
will be obtained from the adoption of
the complete integrated program, and its
potential merits cannot adequately be
judged from the results of using one
phase of it. Some parts (for example, the
soil mixes) will prove helpful if used
alone. Others possibly could lead to ap-
preciable losses (for example, soil treat-
ment, followed by planting with infested
stock). In order to achieve maximum
effectiveness and economic benefit, the
grower must alter his procedures to mesh
with the U. C. system. In this, as in re-
ligion, partial conversion is likely to lead
to backsliding.
The shift of a nursery to the U. C.
system is not as difficult as it may sound.
While numerous production practices
may require modification, the changes
develop logically and progressively.
Change in the attitude of the grower may
be more troublesome, often presenting
the biggest obstacle to success. For this
reason, the easiest and most rapid adop-
tion of the method has usually been by
intelligent, resourceful growers new to
the California nursery business, and
without preconceived ideas. Established
growers who have made the change, how-
ever, usually agree that the results have
been worth the effort. As one elderly
nurseryman phrased it, "It's what you
learn after vou think von know it all
that counts." Minds, like parachutes,
function only when they are open!
With the increasing use of uniform
soil mixes, soil treatments, and healthy
seed or planting stock, and the trend
toward mechanization and the package
marketing of plants, any plan for the
future must take them into account. It
is probable that in some cases a cen-
tralized service for providing a uniform
treated soil may develop, as it has in
England. The soil may then be delivered
into bins at each nursery in a treated
condition ready for use. Alternatively,
the bins may be fitted with a perforated
pipe grid, and the soil steamed in place,
the steam being supplied by the grow-
er's boilers or by a portable steam-
generating service. In any case, nitrify-
ing organisms and those antagonistic to
pathogens can be added.
It is certain that changes will come
rapidly. Sometimes these may be neces-
sary in order to cope with disease prob-
lems, sometimes because of competitive
pressure for cheaper production, at times
for other reasons. The only certainty is
that the trend will always be toward the
least expensive production of the best
possible plants.
[27]
SECTION
Today's Nursery
Problems
Kenneth F. Baker
The California nursery industry
Effect of economic changes
Mechanization and disease control
Causes of disease
.he INFORMATION developed in this
manual concerns the complex problems
of nurserymen and flower producers who
grow crops in prepared soil confined in
flats, pots, cans, beds, or other contain-
ers. Several of the features of California
and its nursery industry have such an
important bearing, directly or indirectly,
on disease control in these crops that they
are considered here.
THE CALIFORNIA NURSERY INDUSTRY
The California nursery industry is an
important part of the agricultural econ-
omy of the state and nation. According
to the 1950 U. S. Census of Agriculture,
the state leads in the production of all
nursery stock. The wholesale value of the
crops grown in 1949 by the 535 produc-
ing nurseries (out of 2.500 in the state)
that filed returns was $10,789,239, or
15.2 per cent of the national total.' This
was more than the next two states com-
bined, California also led in the produc-
tion of ornamental nursers slock (15.0
'That this figure is very conservative is
shown l.\ the L954 farm valuation ($33,324,980)
of nursery stock in \2 southern California coun-
ties. This was tenth among 66 farm commodities
for the area.
per cent of the U. S. total) ; floricultural
plants, rooted cuttings, and other ma-
terial for growing on (17.8 per cent) ;
bedding and vegetable plants ( 16.5 per
cent) ; and lining-out stock (10.9 per
cent) .
There were 6,676 nurseries and other
outlets licensed for plant sales in the state
in 1954-55.
There are about 300 growers of bed-
ding plants, farm plants, and cacti in
the stale. About 80 per cent of the bed-
ding and farm slock is produced in and
south of San Luis Obispo, Kern, and
San Bernardino counties, and about 52
per cent of the stale total is grown within
5 miles of Garden a, in Los Angeles
I 28 ]
County. It is estimated that 2,500,000
flats of bedding and vegetable plants
were produced in the state in the year
ending July 31, 1953. Of this number
1,580,000 flats were sold in the state.2
It was estimated3 that 10,000,000 1-
gallon and 500,000 5-gallon cans were
used in California nurseries in 1952.
In order to produce such quantities
of container-grown nursery stock in Cali-
fornia an enormous volume of special
soil mixes must be used. The bedding-
plant growers use an estimated 39,000
cubic yards annually, and the can nur-
series an additional 55,000 cubic yards.
It is estimated4 that the 2,500 nursery
growers in the state had an average of
one acre per nursery in container pro-
duction. Using a conservative 150 cubic
yards of soil per growing acre per year,
375,000 cubic yards would be required
annually for container growing.
A conservative estimate of the amount
of soil mixes used for container-grown
stock would be 350,000 cubic yards,
with the possibility that it may reach
500,000 cubic yards. This represents the
top soil (1-foot depth) of 217 to 300
acres of land. This does not include flori-
cultural stock grown in beds and benches,
a use which involves additional large
amounts of soil.
Diseases are important
Because much of the propagative ma-
terial produced in California is distrib-
uted over the United States, its disease
status is very important and of more
than local interest. Increasing attention
has, therefore, been devoted to devising
2 Figures in this paragraph are based on data
kindly supplied by J. L. Mather, Manager of
the former Bedding Plant Advisory Board,
Bureau of Markets, California State Depart-
ment of Agriculture.
3 Figures prepared by E. J. Merz, Executive
Secretary, California Association of Nursery-
men, for an O.P.A. investigation of can use.
4 By W. F. Hiltabrand, Nursery Service, Cali-
fornia State Department of Agriculture.
means for producing pathogen-free
plants.
Wide variety of crops
The nursery industry in the state pro-
duces a wide variety of ornamental
crops, including bedding plants, propa-
gating stock (for example, poinsettia and
geranium cuttings), started plants
(roses, azaleas, palms), foliage plants,
succulents and cacti, trees and shrubs,
and herbaceous ornamentals. Pathogen-
free seedlings (pepper and tomato, for
example) are also grown for the vege-
table industry. Thus nurserymen here
grow hundreds of kinds of plants and in
all sorts of combinations. The term
"nursery" as used in California includes
many more kinds of crops than in other
areas of the country, where it generally
refers to woody stock, largely grown in
the field.
This diversity of crops makes it im-
possible to reduce nursery practice to a
rule-of-thumb. In this manual, therefore,
the general methods for disease preven-
tion are outlined, and facts are given
from which a sound program can be de-
veloped for the specific crops, layout,
and location of a given nursery.
Semiarid coastal climate
Nursery production is concentrated in
the counties of Los Angeles (6.9 per cent
of the national total), Alameda, San
Bernardino, San Diego, Riverside, Santa
Clara, Orange, Merced, Tulare, Ventura,
San Joaquin, and Kern, in descending
order. Most of the ornamental crops ex-
cept roses are produced in the cool
coastal zone.
The sunny, generally mild, semiarid,
coastal climate enables the nurseryman
to modify his environment more com-
pletely than is possible in other compa-
rable growing areas. It is more efficient
to control soil moisture through irriga-
tion than by building rain shelters, to
shade plants from the sun than to use
supplemental lights, and to accept re-
[29]
gional temperatures than to heat against
subzero weather. This climate also ef-
fectively limits certain plant diseases.
For example, azalea flower blight causes
severe losses in southeastern states but
is important in southern California only
where a "southeastern climate" is created
by the continuously moist conditions un-
der lath. The possibility of climatic con-
trol in California is great, and the
disease-control problem is simplified by
this fact.
Salinity
There is, however, another side to the
picture. Because of the semiarid climate,
agriculture in California, particularly
the southern part, continually faces a
salinity problem. Most other growing
areas have trouble with salinity only
from accumulation of fertilizers in the
soil due to deficient leaching. Nursery
plants in the southwestern states may be
injured by naturally occurring salts in
the irrigation water or soil, as well as by
too much manure or decomposed leaf
molds and composts (Sec. 4). Although
the nursery industry uses irrigation and
special soil mixes in containers, it has
constant and sometimes severe losses
from excess soluble salts. One of the ad-
vantages of the methods described in this
manual is that they reduce this salinity
problem.
Year-round demand
The climate has still another effect on
the nursery industry here. This is one
of the few regions in the country where
gardening and the demand for nursery
stock continue through much of the year.
Although there is considerable seasonal
variation (fig. 11), the market is pro-
longed and stable as compared, for ex-
August
Fig. 11. Distribution of wholesale sales of bedding plants in California, by months, 1951-52.
Nearly 75 per cent of the stock is sold in the 6 months from February through June, and in
October. (Figures from the former Bedding Plant Advisory Board, Bureau of Markets, California
State Department of Agriculture.)
I 30 1
ample, with that in the northeastern
states with freezing winter temperatures.
This fact has made it profitable to mecha-
nize operations to a greater degree than
in most other areas.
Smog injury
This problem is most acute in the Los
Angeles area, but is appearing elsewhere
as industrialization and urbanization
proceed. Even if reduction of injury to
crops eventually is possible, it will be
expensive, directly or indirectly, and will
be an added economic burden on the
nurseryman. The effects are so serious
that many growers are moving to smog-
free rural areas. When a nursery thus
moves, an opportunity is afforded to de-
velop the new unit along lines of a mech-
anized U. C. system.
Pathogen-free planting stock
There is a general trend toward the
use of pathogen-free propagating mate-
rial. This is evidenced by increasing use
of mother blocks, of certification of bud-
wood, plants, and seeds by various state
agencies, and by the appearance of spe-
cialist propagators. The grower response
to this control of disease at source is
illustrated by the situation of chrysanthe-
mum cuttings. In 1943 a method was
developed by A. W. Dimock for selecting
chrysanthemum stock plants free of Ver-
ticillium wilt, and this was adopted by
an Ohio propagator. In 1949 nearly 26V2
million cuttings were produced in Ohio
(69.5 per cent of the U. S. total) , largely
by this concern ! The use of healthy pro-
pagative stock eliminates one of the im-
portant sources of disease organisms,
and is fundamental to the U. C. system.
Unit containers for marketing
For more effective retailing of plants.
California growers developed the use of
unit containers. Bedding plants are pro-
duced in thin wood veneer, aluminum,
or molded-asphalt packages holding
about a dozen plants. This method of
growing requires a uniform, well-aerated
soil, and freedom from disease organ-
isms. The use of cans for woody plants
in California and Florida has made such
stock available all year for transplanting,
in contrast to the usual short planting
season for stock dug and balled in burlap
or heeled in.
EFFECT OF ECONOMIC CHANGES
Recent economic changes in California
are making it increasingly important to
reduce the cost of fighting disease, and
to avoid the occasional heavy losses they
may cause. These changes also make it
more important to find ways of cutting
labor cost and saving space, and make
mechanization more necessary.
Land values, tax rates, and zoning
restrictions are increasing
Increasing population pressure in the
state is bringing about real-estate devel-
opment, rising land values, higher taxes,
and zoning restrictions. From 1940 to
1950 the population increased by slightly
more than one half, and one third of the
state's dwelling units were constructed.
In the Los Angeles and San Francisco-
Oakland areas the population increased
37.6 and 41.6 per cent respectively, dur-
ing that period. Growers are finding that
these developments collectively create
one of the wrorst pressures they face to-
day, and many are contemplating mov-
ing to rural areas.
On the other hand, the larger popula-
tion will provide an expanding local
market and eventuallv reduce out-of-
[31]
state shipment. The immediate effect,
however, is to sharpen the interest in
techniques, such as soil treatment, that
will reduce cost of production.
In addition to escaping the population
pressures and the increasing air pollu-
tion, a move may be advantageous in
other ways. It provides an opportunity
to clean up a nursery and make a fresh
start along the lines described in this
manual. It is also an ideal time to mecha-
nize, for this almost always involves re-
design of the layout, and is best done
on a new site. In some cases the increased
value of the city land pays a large part
of the c«st of establishing a new, modern,
mechanized nursery. The mechanization
in turn brings reduced labor cost, in-
creased efficiency, and lower production
cost.
The new rural location need not be
on the best level land. Indeed, there are
some advantages, such as lower initial
cost and possible utilization of gravity-
flow operation, in side-hill locations
(Sec. 17) . Present grower experience in-
dicates, furthermore, that distance from
market is not as much of an obstacle as
it once was. Eventually the various pres-
sures may partially offset each other and
hasten the modernization of the Califor-
nia nursery industry.
Labor costs are increasing
Labor costs are increasing rapidly
because of both increased pay scale and
decreased work output. This has led
directly to a growing interest in labor-
saving methods and devices, mechaniza-
tion, and reduction of erratic crop losses.
Returns are decreasing
There are many indications that com-
petition is intensifying in the nursery
business, and that the financial returns
to growers are decreasing. There are two
ways nurserymen can meet this situation.
1. They may reduce production cost
through improved culture, mechaniza-
tion, and reduction of erratic unneces-
sary losses from diseases and similar
factors.
2. They may reduce competition by
growing plants that other nurserymen
find difficult to produce profitably, rather
than those found in most establishments.
The "difficult" crop is usually one that
requires such painstaking, specialized,
or highly skilled techniques for success
that most growers are unwilling or un-
able to produce it profitably. This may
be due to the necessity of controlling
some serious disease, or to the develop-
ment and exclusive retention of a supe-
rior crop variety. Some specialists, for
example, grow pathogen-free propaga-
tive stock of chrysanthemums, carna-
tions, geraniums, or foliage plants. If
the propagator produces healthy stock
at reasonable cost, growers come to de-
pend on him as a source of supply. Other
specialists are developing F1 hybrid
flower and vegetable seed that may be
purchased only from the originator.
However accomplished, such speciali-
zation leads to a limited natural monop-
oly and reduced competition. The more
difficult the problem, the better the job
is done, and the more reasonable the
charges for it, the greater the chance of
thus reducing competition.
MECHANIZATION AND DISEASE CONTROL
For reasons already mentioned, mech-
anization is a present and future fact in
the nursery industry. This in turn im-
poses certain demands, most of which
are in themselves beneficial. Scheduled
production at low cost demands dependa-
ble results. Just as assembly-line manu-
facturing requires that no phase of the
32
process break down, so scheduled mecha-
nized production of plants demands that
all possible chances for error or failure
be removed. Uncontrolled losses from
diseases, such as damping-ofl in seed
flats, must be eliminated or reduced to
unimportance, or the rest of the growing
procedure may be stopped for lack of
material.
Mechanization may lead to bigness,
since some kinds of equipment (for ex-
ample, flat-making or can-filling ma-
chines) can profitably be added only
when the volume has reached a certain
level. This bigness eventually may intro-
duce other problems, as it becomes im-
possible for the man who built the suc-
cessful enterprise to maintain personal
supervision. The daily application of his
knowledge, experience, and foresight
often is the price of maintained success,
and very large nurseries may exhibit
slackness or inefficiency for this reason.
Increase in size places ever greater em-
phasis on assured control of diseases,
insects, and soil problems.
CAUSES OF DISEASE
Many explanations are offered for
failure of a nursery crop, and these often
confuse rather than clarify. Thus it is
said that flats of seedlings have been wa-
tered too much or too little, the seedlings
were planted too deep or too shallow,
the weather was too hot, the plants were
too soft or too hard, or came from a
poor lot of seed, or were grown in the
wrong soil mix. In most cases investiga-
tion has revealed that pathogens had
caused the disease, and that the condi-
tions blamed had merely aggravated the
trouble.
This confusion is understandable in
view of the complexity of some of the
situations encountered. Perhaps the com-
monest example in southern California
is the damping-off-salinity complex. A
grower who uses untreated composted
soil that is high in both soluble salts and
damping-off fungi truly faces a dilemma.
If he keeps the soil on the dry side to
reduce fungus attack, the plants will be
injured by the increasing concentration
of salts. If he tries to avoid salinity in-
jury by leaching out the salts, or by keep-
ing the soil wet to dilute them, favorable
conditions may be created for damping-
off fungi (fig. 35). Indeed, this situation
sometimes is seen in a single flat contain-
ing poorly leveled soil. The water runs
to the low parts and leaches them, and
the seedlings there grow well until they
damp-off. In the high parts of the flat,
the seedlings are stunted and hardened
by salt concentration, but have little
damping-off. The only real solution to
this situation is to keep the salinity at a
low level, and to treat the soil to free
it of pathogens.
Growers may be further confused be-
cause many factors that may aggravate
disease once it appears, will not initiate
it. It is one purpose of this manual to
explain the action of the several factors
in this disease complex so that growers
will have a rational basis for its under-
standing and prevention.
[33 1
SECTION
Damping-OfT and
Related Diseases
Kenneth F. Baker
D
Development of methods for disease control
Nursery diseases and their pathogens
The Rhizoctonia story
The water molds, Pythium and Phytophthora
Other organisms that cause nursery diseases
Control of nursery diseases
iseases OF California nursery crops
range from seedling damping-off to leaf
spots and stem cankers, fire blight and
crown gall, root rots and flower blights.
Since this manual is concerned with dis-
eases in relation to nursery soil in con-
tainers, its coverage is largely restricted
to damping-off and related diseases of
propagative material. These pathogens
necessarily involve soil, live in it, or use
it as a base for attacking crops.
Excluded are diseases specific to single
crops, those in which the causal organ-
isms are only incidentally associated
with soil, and those that parasitize so
slowly that symptoms are largely shown
in the post-nursery phase. Included, how-
ever, are some of the most insidious,
omnivorous, tenacious, and destructive
pathogens, causing some of the worst
headaches of the nurseryman.
DEVELOPMENT OF METHODS FOR DISEASE CONTROL
The parallel development of disease
control in plants and man is instructive.
In early times (and in backward areas
even today) lack of understanding of
disease led to invocation of supernatural
causes. Treatment involved atonement
to angry deities, and therefore involved
application of unpleasant noxious mix-
tures to man and plants. Surgery, per-
formed only when imperative and with-
out regard to sanitation, was usually
fatal.
During the mid-nineteenth century,
after microorganisms were shown to
cause disease, antiseptics came into use
to destroy pathogens on or in plant or
man. The mortality from disease and
surgei \ fell sharply. 'Flic comparable use
of sprays on plants developed rapidly,
and still provides one of the principal
methods of plant disease control.
Toward the end of the nineteenth cen-
tury the concept was gradually accepted
that preventing the introduction of or-
ganisms was better than trying to destroy
them on or in the host by antiseptics.
This gave rise to the aseptic surgery of
today, with emphasis on sterilization of
equipment and on general cleanliness.
Preventing the introduction of pathogens
is also the thesis of this publication on
nursery diseases, expressed in the motto,
"Don't fight 'em, eliminate 'em." This
emphasizes using soil and plant mate-
rials free from disease organisms, and
using cultural techniques which will keep
[34]
them that way. This is the central core
of the U. C. system.
In the present day, antibiotics have
revolutionized many aspects of medicine
and surgery. They may conveniently be
injected into animals, but this has not
been very successful with plants. They
have only a local fungicidal effect when
sprayed on plants. Since antibiotics
rapidly break down when introduced
into soil, it appears that best results there
may come from the production of them
by the appropriate organisms, in place.
Difficulties must be resolved before this
method of disease control comes into
wide use, even under the uniform con-
trolled conditions of the nursery. This,
then, provides another reason for uni-
formity of soil mix, soil treatment, and
handling. The use of antagonistic soil or-
ganisms and the adoption of some uni-
form soil system may enter general
nursery practice simultaneously, rein-
forcing and modifying each other in the
process; these topics are discussed fur-
ther in sections 5 through 7, and 14.
NURSERY DISEASES AND THEIR PATHOGENS
Types of Diseases
Damping-off of seedlings
The several types of damping-off may
occur separately or simultaneously in a
seedbed.
1. Seed may decay before it germinates
(the seed-decay phase) or the seedling
may rot before it emerges from the soil
(preemergence damping-off, fig. 12).
Losses of these types are usually blamed
on defective seed because of the poor
emergence, but are often caused by a
number of different fungi.
2. Seedlings may develop a stem rot
near the soil surface and fall over (fig.
13). This postemergence phase, the most
conspicuous type of damping-off, is
caused by Rhizoctonia or by the water
molds.
3. Some seedlings may be so tough, or
the environment so unfavorable, that the
stems may only be girdled, and the plants
remain alive and standing (figs. 1 and
14). Although this wire-stem or sore-
shin type is less striking than the former,
it is just as destructive because the plant
is stunted and eventually dies. It usually
is caused by Rhizoctonia.
4. Another postemergence variant,
commonly caused by water molds, is that
in which the rootlets rot from the tips
(fig. 15) ; the fungus usually progresses
up to the stem, and the plant dies.
Top rot of seedlings
or cuttings
Under moist conditions Rhizoctonia,
or sometimes Phytophthora, may spread
from leaf to leaf, or stem to stem, through
the tops of seedlings or cuttings (fig.
16). It may rot the tops down to soil
level, and frequently the crown and roots
are uninjured. The fungus may originate
from the soil, spreading up the first
plants, but remain aerial thereafter.
Cutting and stem rot
Cuttings may rot progressively from
the cut end (fig. 17), the root bases, the
wounds of disbudding (rose) or remov-
ing of basal leaves (gardenia), or from
dead leaf bracts (geranium) . A variant of
this is the rot of the propagative piece of
Dieffenbachia cane by Pythium or by
soft-rot bacteria carried over in tiny
lesions from the mother cane. Similarly,
the organisms causing bacterial stem rot
of geranium, bacterial wilt of carnation,
and bacterial blight of chrysanthemum
may be transmitted unnoticed in the
vascular system of the cutting and cause
its eventual decay.
[35]
Root rot of mature plants
The roots of nursery plants in pots,
flats, or gallon cans may rot (much as
in fig. 15) and cause the death of the
plant. The tops may die slowly, with yel-
lowing and dropping of leaves beginning
at the base, or the leaves may rapidly
wilt and die, remaining attached to the
plant. The rate of symptom expression
in the tops is dependent on the rapidity
of root decay. The water molds usually
cause this disease, and the soil moisture
is important in determining the rate of
root decay.
Time and Severity of Losses
The loss to the nurseryman may be
immediate, as in damping-off or top rot
of seedlings. It may, however, be delayed
and cause slow loss of infected plants,
as in root rot caused by water molds
when plants are grown under relatively
dry conditions. It may cause the death
of plants in 5-gallon cans several years
after propagation and infection, as is
often the case of Choisya infected with
water molds.
Loss may even be so delayed that it
will occur after the plant has been sold
and planted in a home yard. Nurserymen
often do not learn of such a loss, or may
feel that it is beyond their responsibility.
Since the soil becomes infested from such
a plant, other clean replacements are
likely to become diseased and likewise
die. Although a very few nurserymen
may take the view that these repeated
losses will promote plant sales, the gross
effect undoubtedly will be harmful to the
industry. The buyer may become a dis-
couraged gardener and poor customer,
may change nurseries in order to find
better stock, or may learn the facts and
become actively antagonistic. It is cer-
tain that the sale of vigorous pathogen-
free plants is one of the best ways to
build a good reputation and promote
sales, both for a single nursery and the
industry. Thus the direct or immediate
[36]
losses and the indirect or delayed ones
are of equally great importance to nur-
serymen.
Losses from these types of disease in
nurseries may be very great. Frequently
50 per cent or more of some types of
plants (Choisya, succulents, cacti, Cali-
fornia "natives") die before sale. When
it is considered that the margin of profit
in the nursery business is fairly small
and becoming smaller, a severe disease
loss may be disastrous. An average loss
of 1 to 10 per cent from diseases would
be a conservative estimate. This must be
a severe drain on the slender margin of
profit in many nurseries, and probably
causes many of them to operate at a loss,
at least on some items.
Relative Importance
of Pathogens
In California, as apparently in much
of the world, the principal cause of the
diseases mentioned is a fungus (Rhizoc-
tonia solani) commonly, though not af-
fectionately, called "rhizoc." In the past
10 years this fungus has become increas-
ingly important as a pathogen of flower,
nursery, vegetable, and field crops in
southern California. While the reason for
this increase is not known, the pathogen
is rapidly becoming the most important
single fungus causing crop disease in
that area.
Of less general importance, the water
molds (Pythium and Phytophthora spp.)
may be locally damaging.
Other fungi cause infrequent losses to
seedlings and cuttings, but are of minor
importance.
It is the purpose here to explain and
illustrate the nature of these various
fungi, and how they survive and spread,
so that a grower may better understand
what is happening, and better plan his
preventive program. Rhizoctonia is dis-
cussed in detail as the principal example,
and discussions of less important organ-
isms refer to it.
[37]
THE RHIZOCTONIA STORY
Recognition of Rhizoctonia
Diseases
It is reasonably certain that rhizoc is
the cause of the disease when (1) the
decay originates near the soil surface
(fig. 13) , rather than at root tips as with
the water molds (fig. 15) ; (2) coarse
brown fungus mycelium is seen, with the
aid of a good 10 to 15x hand lens, on
the decayed parts (figs. 17, 18, and 27) ;
(3) there are soil particles clinging to
the tough fungus strands after the seed-
ling is shaken to remove the soil mass
from the roots (fig. 18) . Few other fungi
{Helminthosporium cactivorum on cac-
tus is one of the exceptions) have been
found to simulate these features of
Rhizoctonia; the fungi can of course
easily be differentiated by growing them
on culture media.
Cuttings may rot progressively up-
ward when infection has occurred below
soil level (fig. 27). In humid propagat-
ing cases Rhizoctonia often spreads as a
coarse web through the tops of some
plants (for example, Araucaria cuttings,
azalea cuttings and grafts) , matting them
together (fig. 16).
The Rhizoctonia Fungus
Rhizoctonia solani is a simple plant
consisting of brown threadlike branch-
ing mycelium. The presence of this
characteristically branching mycelium
(fig. 19, top) on, and particularly in,
diseased tissue affords a rapid labora-
tory microscopic diagnosis for the
fungus. In the soil these filaments grow
between the particles and in bits of or-
ganic matter (highly magnified in fig.
20). Sometimes these strands fuse to-
gether and form visible clumps (sclcro-
lia. fig. 19. bottom) that are long-lived
and survive drying. Thus, infested soil
and flats ma\ be stored dry for 6 months
01 more without killing the parasite.
When the fungus grows into contact with
a seedling (figs. 12 and 13), its my-
celium grows over the surface and pene-
trates the tissues (fig. 28), digesting
them for its own nutrition, and thus pro-
ducing the disease.
The fungus is a relatively unspecial-
ized parasite, able to attack many kinds
of plants, although there are important
differences in this ability between strains
of the fungus (Sec. 15).
Spread of the Fungus, and
Preventive Measures
Under conditions of plant propaga-
tion, Rhizoctonia produces spores ex-
tremely rarely or not at all. For all
practical purposes there is no air-borne
stage, and spread occurs by mechanical
transfer of mycelium and sclerotia in in-
fested soil particles and infected plant
tissue. These bits of mycelium resume
growth in the new location. This is of
great significance in control procedures.
Rain or watering
During rain, overhead irrigation, or
watering of flats and beds in which the
fungus occurs, bits of soil containing its
strands commonly are spattered to near-
by uninfested plantings (fig. 21).
Dipping cuttings
Similarly, spread may occur from dip-
ping cuttings in water or in hormone
solutions. Since water is an efficient car-
rier of many kinds of pathogens, it
should not be used as a dip in cutting
treatments; any materials should be
either dusted or sprayed on instead.
Soil in watering hose
The soil under benches in greenhouses
often is infested with Rhizoctonia. When
the hose is dropped on the ground after
use, bits of infested soil may get into the
[38 1
[39]
open end (fig. 22) and be washed into
a clean planting when next used. This
is the principal reason why heavy disease
losses frequently occur in beds at points
near the faucet. Nozzles should be hooked
on the side of benches when not in use
to keep them up off the ground (fig.
8).
Infested containers
Rhizoctonia very commonly lives over
between crops in bits of soil on the wood
and in the corner joints of flats (fig. 23) .
When clean or treated soil is placed in
such a flat, and irrigated after planting,
the fungus resumes growth and causes
damping-off in the corners (fig. 23) or
along the sides. It is carried over in
benches and cold frames and on pots in
the same manner. Flats and benches
should be treated with steam or chemi-
cals (Sec. 12) after each use to prevent
carryover of pathogens.
Infested tools and equipment
Exposed surfaces and cracks in tools
and equipment such as shovels, trowels,
dibbles, replanting tools, and wheelbar-
rows also afford a place for survival and
spread of the fungus (fig. 24). After
use in infested soil, tools should be
dipped for a few minutes in a crock con-
taining 1 gallon of commercial formal-
dehyde to 18 gallons of water (fig. 7) ;
they may be rinsed in water and used
without delay.
Grower's hands and feet
The fingers of the grower may also
carry bits of soil and the fungus from
flat to flat while testing for moisture or
knocking plants out of pots for root ex-
amination. A green thumb may actually
be the black hand for seedlings! This
hazard is minimized by having only
treated soil in clean flats in the green-
house range.
Equally dangerous and unfortunately
common is the practice of walking on
the edges of flats in ground beds while
[40]
watering, for infested soil particles often
drop from the shoes into clean flats.
Placing containers on ground
It is poor practice to place clean flats
or cans on ground beds at all; infested
soil may be kicked or splashed into flats,
or the roots grow through the bottom and
become infected, the fungus then spread-
ing to the plant above. Outdoor beds
where flats are to be placed may be
drenched with formaldehyde (1 pint of
commercial formaldehyde to 61/4 gal.
water) at % gallon per square foot of
surface. They must be kept moist and
aerated for 10 to 14 days before use
(Sec. 11). Two by four timbers treated
with copper naphthenate (Sec. 12)
placed flat on the ground will elevate the
flats sufficiently to provide inexpensive
and fairly effective protection. If flats
are placed on polyethylene sheets laid
on the ground, protection is also af-
forded. Some nurseries pave the area
with asphalt.
When treated flats are stacked on un-
treated ground the bottom one should
be discarded; at the minimum it should
never be stacked among other clean flats.
A good practice is to place stacks of
treated flats on clean wooden pallets to
keep them off the ground.
Unsterilized covers
The use of old unsterilized canvas or
sacking over seed flats is a common
source of infestation of clean soil (fig.
25). Unsterilized lath frames placed over
flats may also be dangerous. All such
materials should be steamed or treated
chemically before re-use.
Infected plants or seeds
Rhizoctonia may also be carried to
clean soil by infected (but healthy ap-
pearing) plants or seed. With some crops
(tomato, eggplant, pepper) the fruit in
contact with the soil may be slightly de-
cayed by the fungus, which then develops
on and in some of the enclosed seeds
27
CLEAN SOIL
28
[41]
I fig. 26). Zinnia seedheads piled to dry
on canvas on the ground may similarly
be invaded and the seed infected. Such
transmission of Rhizoctonia fortunately
is not known for most kinds of seeds.
It is usual practice to salvage seedlings
or cuttings from the margins of an area
of damping-off in seed pan or propagat-
ing bench, in the mistaken notion that
only decayed plants are infected. Ac-
tually infection, under some conditions,
may occur a few days before symptoms
appear. To transplant such stock to clean
soil is to transfer the Rhizoctonia fungus
(fig. 27). A wise precaution is to cover
the diseased areas with inverted tin cans
before beginning to transplant, making
sure that the can extends well beyond
the margins.
Root divisions or basal cuttings of
plants such as chrysanthemums grown
in infested soil commonly carry the
fungus to the new planting or propaga-
tion bed (fig. 27). This carryover can
largely be avoided by using only cuttings
from tips of stems a foot or more above
the soil, since the fungus is not carried
to that height by splashing water.
The parasite invades the stems of the
seedling or cutting, and once inside
the tissues is very well protected from
any fungicide (fig. 28). Because of this,
it is not possible to cure a diseased
seedling by fungicidal application. Em-
phasis must be on prevention of infec-
tion. It is possible, however, to prevent
spread of Rhizoctonia from a small in-
fection in a flat by "spot treatment" of
the diseased area (Sec. 11).
Conditions Affecting
Disease Severity
The severity of attack by Rhizoctonia
is conditioned by the susceptibility of
the host, the inoculum potential, and a
number of environmental conditions.
Some examples of these factors follow.
In general, those conditions unfavorable
to the plants without being loo detrimen-
tal to the fungus will give severe disease
losses. The more unfavorable the condi-
tions are to the plant, without drastically
reducing growth of the fungus, the
worse the disease will be.
Susceptibility of the host
Peppers consistently suffer heavier
losses from Rhizoctonia damping-off
than do tomatoes, and pansies or stocks
are more sensitive than calendula. The
sensitivity of the plant to the environ-
mental conditions given below must also
be considered.
Inoculum potential
The quantity of Rhizoctonia in the soil
determines the potential severity of the
disease and, to some extent, the effective-
ness of control procedures. For example,
if the fungus is present in sufficient
quantity in soil, it is almost impossible
to control damping-off by chemical
treatment of the seed or by treatment of
the soil by the dilute-formaldehyde
method (sees. 11 and 15). The environ-
mental conditions determine whether the
potential severity is attained.
Soil salinity
Soil salinity (Sec. 4) causes, at dif-
ferent concentrations, suppression of
germination, stunting of plants, killing
of the margins or entire blades of leaves,
or death of seedlings. Experiments at
Pennsylvania State University showed
that sublethal salinity increases severity
of Rhizoctonia damping-off. This may ex-
plain the increasing importance of this
fungus in southern California in the dec-
ade after 1944, when deficient rainfall
greatly increased the salinity problem.
Nitrogen and carbohydrate
status of plant
The higher the relative level of soil
nitrogen, the softer the plant growth will
be. Above a certain level this increases
susceptibility to Rhizoctonia damping-
off. Favorable light for the plant enables
[42]
it to produce sufficient carbohydrates for
thickened cell walls and sturdy growth.
To a considerable extent, nitrogen sup-
ply and carbohydrate level (sunlight)
offset each other. A plant grown at a
barely adequate nitrogen level in sub-
dued light would be nitrogen-deficient
in bright light, and one with adequate
nitrogen in full sun would have too much
in reduced light. Thus, light must be
considered in determining an adequate
nitrogen level. Generally, high-nitrogen
or low-carbohydrate seedlings are sus-
ceptible, whereas the hard plants of low
nitrogen or high carbohydrate are more
resistant.
Watering
Application of water affects plant suc-
culence and susceptibility, in part
through affecting nitrogen intake. At-
tack by water molds can be reduced in
severity by maintaining the soil as dry
as will permit plant growth, but this will
not inhibit Rhizoctonia. Rhizoctonia con-
trol through reduced watering probably
is mainly operative on the plant rather
than on the fungus.
Soil temperature
The growth of both plant and fungus
is affected by soil temperature, but the
effect is often unequal in degree and
range. Thus, a strain of Rhizoctonia may
severely injure peas (a low-temperature
crop) at high, but do little or no damage
at low soil temperatures, and attack
beans (a high-temperature crop) at low
but only slightly at high soil tempera-
tures.
Depth of planting
Deep planting of seed delays emer-
gence and keeps the seedling in a sus-
ceptible state (devoid of light and there-
fore low in carbohydrate) for a long
period of time. This naturally favors
incidence of damping-off.
Reduced vitality of seed . . .
causes delayed emergence of the seed-
ling, with much the same effect as deep
planting. Old weak seed may have more
trouble from damping-off than new seed
of high rapid germination.
Rhizoctonia Infections on
Mature Plants
Mature plants as well as seedlings are
affected. It is a mistake to regard damp-
ing-off and cutting-decay fungi as limited
to juvenile plants, although their damage
may be greatest there. Rhizoctonia
causes, in addition to seedling damping-
off, serious losses from wire-stem gir-
dling of mature stocks, peppers, cabbage,
and other plants in the field, as well as
from stem rot of mature carnations,
pansies, and petunias. It has also caused
serious rot of the deep roots of nursery
roses, asters, and camellias. The water
molds may even assume their greatest
importance in the postnursery growth.
Transplanting apparently healthy, but in-
fected, seedlings to the field or bed does
not end the matter, for they frequently
die later and give an irregular stand
(fig. 29), as well as infest the soil with
the fungus.
Temporary suppression
is not control
Some measures aim at suppression of
the fungus in seedbed or propagation
frame by the use of:
1. A sand or sphagnum moss surface
layer;
2. Reducing watering;
3. Increased aeration of seedlings;
4. Reduced use of nitrogenous fertilizers:
5. Increased light;
6. Fungistatic drenches (for example.
PCNB), or even fungicides having
poor soil penetration (Arasan, cap-
tan).
[43]
These palliative treatments may be
quite effective when skillfully applied,
and therein lies the danger.
The fungus may be suppressed under
the controlled conditions of the seedbed
or flat, only to appear again when the
plant is in the pot, the 5-gallon can, or
in the largely uncontrollable environ-
ment of the commercial or home plant-
ing. Under these conditions the suppres-
sive measures may be ineffective or un-
economical, and it finally becomes
evident that the loss has been merely
postponed until the investment is greater.
(see also "The Water Molds," below).
Strains of Rhizoctonia
Rhizoctonia strains differ in response
to various environments and hosts. As
pointed out in Section 15, it is unsafe to
assume that all strains of Rhizoctonia
solani, which are fairly common and
widespread, are alike and that the dis-
tribution of diseased stock is therefore
unimportant. In comparison with highly
specific soil organisms, such as the wilt
fusaria, which attack only a single species
of plant, this fungus is unspecialized ;
but there are differences in pathogenicity
among strains of Rhizoctonia sufficient
to be of great economic importance.
There are saprophytic forms of R. solani
in most field soils, but this is no excuse
for bringing in virulent pathogens on
the stock to be planted.
In addition it must be considered that
diseased stock, because it is already in-
fected, will suffer more rapid and severe
injury than that infected in the field.
Planting diseased stock also serves to
increase the quantity of pathogen present
and to distribute it more uniformly
through a field.
For all of these reasons it is important
that the stock produced not be merely
disease-free (that is, healthy appearing),
but that it be pathogen-free as well.
THE WATER MOLDS, PYTHIUM AND PHYTOPHTHORA
Types of disease
Damping-off caused by Pythium or
Phytophthora usually starts at tips of
main or lateral roots but may rapidly
involve all parts below ground (fig. 30)
and thus cause the seedlings to fall over.
These organisms also commonly cause
decay of seeds or seedlings before they
emerge from the soil (as in fig. 12).
The fungi
The fungus mycelium on the roots is
fine, colorless, and difficult to see with a
hand lens; it is so delicate that it does
not hold soil particles, as does that of
Rhizoctonia. The mycelium grows be-
tween soil particles and in organic mat-
ter l as in fig. 20) through the top several
inches of soil; it is therefore in a posi-
tion to invade root tips. These fungi
generally are damaging to plants only
when the soil is very wet, hence the name
"water molds." Rhizoctonia, on the other
hand, develops best under conditions of
moderate soil moisture.
Under favorable conditions the water
molds produce in soil and on its surface
microscopic saclike structures (zoos-
porangia),from which emerge numerous
swimming spores (fig. 31). These swim
about in water for a time before develop-
ing into mycelium, which penetrates a
seedling root.
In diseased plants these fungi com-
monly develop thick-walled oospores
(fig. 32), which are long-lived and very
resistant to drying. These spores are use-
ful in rapid laboratory microscopic ex-
[44]
amination of suspected roots for this
group of fungi, which frequently are
difficult to isolate in culture.
Spread
The water molds are spread in the
various ways just described for Rhizoc-
tonia, and in addition the swimming
spores may be scattered in splashing
drops, irrigation water, and so on. These
motile spores may develop in standing
water in small reservoirs and irrigation
canals, and be spread by using such in-
fested water. They are not, however,
found in city water supplies in Cali-
fornia.
The oospores are released to the soil
by decay of the plant, and may function
there in the same way as sclerotia of
Rhizoctonia. Therefore, the water molds,
despite the sensitivity of the mycelium
and motile spores to drying, may survive
in dry soil for several months and be
spread in dry soil or on tools or flats.
The mycelium, motile spores, or the
resting spores of water molds are not
carried by air currents. The water molds
may be introduced to clean soil with in-
fected seedlings and cuttings. Phytoph-
thora also is known to be carried in the
seed of some types of plants.
Effects on mature plants
The water molds are important in
postnursery phases of growth as well as
in the seedbed. There is increasing evi-
dence that water molds, as well as some
other organisms, may retard root de-
velopment (and thus plant growth)
without invading tissues. Because of this
effect, as well as actual root decay, many
of the water molds are dangerous both
in the nursery and postnursery phases.
Phytophthora cinnamomi may cause de-
cay of tiny heather cuttings and the
death of large plants in cut-flower fields;
it may cause loss of avocado rootstock
seedlings in the nursery, and of large
trees in the grove.
[45]
Gravatt (1954)1 has recently called
attention to the fact that Phytophthora
cinnamomi is an introduced danger to
native stands of chestnut, shortleaf pine,
Douglas fir, and Port Orford cedar, as
well as many cultivated plants, and that
it is widely spread with nursery stock.
Control procedures should be employed
that eliminate these fungi, rather than
those that temporarily suppress them.
OTHER ORGANISMS THAT CAUSE NURSERY DISEASES
Other organisms than Rhizoctonia and
the water molds may sometimes cause
diseases of nursery crops. In addition,
some other seedling diseases, such as
downy mildew of snapdragon or bac-
terial leaf spot of delphinium, may be
confused with damping-off. It is possible
to discuss here only representatives of
such seedling diseases. Because of the
difficulty of distinguishing some of these
less common troubles, the grower should,
when in doubt, consult the local farm
advisor. The policy, already discussed,
of eliminating the pathogen should be
adopted whenever possible.
Gray mold
Under certain circumstances Botrytis
cinerea may cause losses in flats of a
wide variety of plants. The fungus is able
to infect only through dead or dying
plant parts under continued cool, moist
conditions, and works from the top
downward. It starts in (1) seedlings in-
jured by other causes, such as fertilizer
or salinity burn or water dripping from
the greenhouse, or (2) from foreign
plant parts (for example, petals) that
have fallen on the seedlings. The fungus
spreads to adjacent seedlings, which
finally become covered with a woolly
gray growth (fig. 33). This fungus can
be identified by this growth, by its re-
striction to cool, moist conditions, and
by the fact that it begins with injured or
dead parts.
' Citations given in the lex! by author and
• late will be found, listed by sections, under
"References" in the Appendix.
It is possible to prevent this disease
by growing seedlings under either drier
or warmer conditions and avoiding in-
juries to the plants, despite the fact that
the fungus is extremely common and is
air-borne.
The cottony-rot fungi
Sclerotinia sclerotiorum and S. minor
sometimes cause damping-off of seed-
lings. They attack healthy plants and
under cool, moist conditions spread very
rapidly through the flat or seedbed. They
are easily recognized by the dense, white,
cottony growth in which are found
numerous hard black sclerotia (fig. 34).
These fungi most commonly occur as soil
organisms, being spread and controlled
in much the same way as Rhizoctonia.
The sclerotia may also sometimes be
spread with the seed. A shooting-spore
stage is rarely formed under greenhouse
conditions, so the air-borne spores may
be ignored there. Under field conditions,
however, they are rather commonly de-
veloped, and infection by the air-borne
spores gives rise to the white blight of
aerial parts of some crops (for example,
stock, petunia).
The aster-wilt fungus
Fusarium oxysporum f. callistephi
may cause damping-off in seed flats or
beds. It attacks no other plant than the
China aster and causes damping-off only
in very heavily infested or warm soil.
The seedling rots from the root upward
and falls over, without showing any
fungus growth. Recognition of this
[46]
trouble may require the assistance of the
farm advisor, but it should be suspected
if losses are restricted to aster, if the soil
is known to be infested with aster wilt
and has been held at temperatures above
70° F, or if untreated seed has been
planted. Control of this disease is by soil
and seed treatment.
Nematodes
These animals may cause (1) swell-
ings on the roots (root-knot nematodes,
Meloidogyne spp.) , (2) roots to be killed
or lesions produced on them (Pratylen-
chus spp. and many other surface-feed-
ing types), (3) stem enlargement or
necrosis (stem and bulb nematode, Dity-
lenchus spp.), and (4) dead areas in
leaves (foliar nematodes, Aphelenchoides
spp.). They are tiny, colorless, wormlike
animals barely visible to the naked eye,
and are spread in the ways already de-
scribed for Rhizoctonia. There are many
types of soil-inhabiting nematodes, and
a great deal of specialized information
has been published about them. For our
purposes here, however, it is important
that the same general control procedures
(clean soil — see sees. 8 and 11; clean
stock — see Sec. 13; sanitary practices —
see sees. 1, 12, and 14, as well as this
one) outlined for fungi in this manual
will prevent their damage.
Other seedling diseases
Other diseases are frequently confused
with damping-off. For example, the
downy mildew ( Peronospora antirrhini)
of snapdragon may attack the leaves and
stems of seedlings, killing them to the
ground. The leaves have a dull green
color, become rolled, and have a dense,
dirty white, mealy fungus mass on the
undersurfaces. Seedlings killed to the
ground frequently will resprout and de-
velop new tops, a condition that does not
occur with damping-off. The disease oc-
curs only under very moist cool condi-
tions, and may be prevented by growing
in a drier or warmer greenhouse. The
application of a Parzate dust has proved
effective in control.
The bacterial leafspot of delphinium
(caused by Pseud omonas delphinii)
sometimes kills seedlings. Infections start
as tiny watersoaked spots in the leaves
that may become black or, under very
moist conditions, may spread through the
whole plant. The disease spreads down-
ward from the top, and is thus distin-
guished from damping-off. If the disease
is controlled by a spray of dilute Bor-
deaux mixture, the seedlings will sprout
again.
[47]
CONTROL OF NURSERY DISEASES
Disease organisms may be introduced
into a clean planting through the medium
of (1) the soil, (2) the seeds, cuttings,
or other planting material, and (3) bits
of soil on such things as tools, flats, and
hoses, or splashed by water.
Damping-off and related nursery
diseases are most effectively combated
when preventive treatment aims at
elimination of the fungus from the above
sources before beginning the given oper-
ation. Such a complete program demands
foresight and planning, but has been
successfully adopted in several nurseries.
Control Measures Needed
Treat soil
Steam or chemically treat all soil
mixes and propagating media to destroy
disease microorganisms and weed seeds
in them. This preferably should be done
in the container (for example, flat or
bed) where it is to be used. See sections
8 and 11 for details of methods.
Use pathogen-free seed
and planting stock
There is no point in planting infected
stock in treated soil, nor is there any
excuse for planting healthy stock in in-
fested soil. Seed may be heat- or chemi-
cally treated to free it of pathogens.
Vegetative propagative material can be
freed of disease organisms in various
ways, and such stock is already available
for a number of commercial crops. See
Section 13 for details.
Follow a sound
sanitation program
To prevent contamination of the clean
plant in treated soil it is necessary to
disinfest tools, flats, and other con-
tainers (sees. 1 and 12). Handling prac-
tices that spread disease organisms
should be discontinued or modified (see
'The Rhizoctonia Story," above). More
direct ways for coping with this recon-
tamination problem are under study
(Sec. 14).
Spot treatments for
limited infestations
When a small area of seedling disease
appears in a valuable bed or flat, its
spread may be stopped by application of
a chemical drench (Sec. 11) and the un-
infested plants saved. In all stock that is
to be grown on for extended periods or
is to be planted in uninfested field soil,
this method is beset with many hazards,
as already explained. The most intelli-
gent use of spot treatments is for confin-
ing disease to a specific area in a grow-
ing crop as a means of reducing loss,
particularly when the land in which the
seedlings are planted is to be subse-
quently treated to destroy the infestation.
Relation to
Certification Programs
In California, nurseries which meet
the high standards of freedom from dis-
eases and pests required by Rules of the
State Director of Agriculture may use
intercounty nursery stock certificates
("pinto" tags) on shipments within the
state. Shipments bearing these certifi-
cates need not be held for inspection at
destination, as would otherwise be neces-
sary. One of the requirements of the
Director is that certain plants must be
grown in treated soil and adequately
protected from reinfestation in order to
be eligible for movement in shipments
bearing such certificates.
In effect, these certificates provide an
indication that the nursery is using ap-
proved disease-prevention practices. The
program is voluntary, but high standards
must be maintained if the certification is
[48]
to be kept. Many nurseries treat all soil
used, whether or not it is required, and
this permits continued use of the certi-
ficates. Clean soil is important in any
certification program.
Benefits from Elimination of
Diseases
When a disease is eliminated from a
nursery, production becomes easier,
more certain, and less expensive.
Increases growth potential
of crop
Many of the "secrets" of growing
various crops are simply practices, ar-
rived at by costly trial and error, which
enable a grower to live with a disease.
In almost all cases, however, the produc-
tion would be improved if the disease
were not present, because of the in-
creased growth potentialities of the crop.
Thus, V erticillium wilt of chrysanthe-
mum can be controlled by using resistant
varieties, but more and in some cases
better varieties are available if this is not
the determining factor. Control of this
disease has in this way undoubtedly
speeded the adoption of year-round pro-
duction. Some growers have been able
to produce susceptible varieties in in-
fested soil by very careful and costly
watering, but are now adopting the
preferable soil treatments. Similarly,
losses from Phytophthora root rot of
heather can be reduced by minimal
watering, but plant growth is retarded
and more skill is required in watering
than when the disease is absent.
Increases environmental
tolerance of crop
The presence of a disease often dras-
tically restricts the range of variation in
some environmental factor that is toler-
ated by a crop. Elimination of the disease
in such cases therefore permits use of
the full growth range of the crop, and
makes for easier, less restricted culture.
In southern California nurseries, the
problems of salinity and damping-off
illustrate the confusion which often
arises when disease prevention is at-
tempted through controlling the soil
moisture (fig. 35). In the absence of
salinity and of parasites, seedlings grow
over a wide moisture range. If salinity
exists, the soil should be kept moist (Sec.
4) and, if water molds are present, it
should never be watered excessively. The
presence of Rhizoctonia complicates the
situation, since it generally is favored by
intermediate moisture levels, the same as
the seedlings. Because uncertainty fre-
quently exists as to the exact problem or
problems involved, it is understandable
how confusion has arisen from attempts
to solve these problems by water control.
The only real answer to this complex
situation is the elimination of disease,
rather than trying to "live with it".
A similar difficulty involves the pro-
duction of China asters (fig. 36). Fusa-
rium wilt is favored by soil temperatures
of 60° to 85° F, and most favored at
about 75° to 80°. Growers who at-
tempt to reduce wilt losses by growing in
the cool season or along the coast have
sustained heavy losses from Botrytis and
Rhizoctonia crown rot. The plants re-
main in the rosette stage under short-day
conditions, the shaded lower leaves die,
and moisture is favorable for Botrytis
and Rhizoctonia. The best answer is to
eliminate Fusarium and Rhizoctonia,
and to grow the plants during warm
weather and long-day conditions.
Benefits are greatest
with best culture
The better the culture of a crop the
greater will be the benefit from elimina-
tion of disease, because each healthy
plant will produce greater financial re-
turn than under poor culture. For this
reason new methods of disease control
are usually taken up first by, and prove
most beneficial to the better growers.
[49]
No parasites or salinity
Salinity , Rhizoctonia , Water molds
Salinity only
O
O
z
<
Salinity, water molds
Water molds only
Salinity, Rhizoctonia
Rhizoctonia only
Water molds, Rhizoctonia
Dry
Moist
Dry
Moist
SOIL MOISTURE
SOIL MOISTURE
Fig. 35. Diagrams illustrating some of the difficulties of preventing damping-off and salinity
in seedling production through controlling the soil moisture. The shaded areas indicated the soil-
moisture levels which result in best growth because of least damage from salinity and damping-
off due to Rhizoctonia or water molds, separately and in various combinations. Each of these
three factors restricts the levels of moisture that may be maintained with safety, and the presence
of all three essentially precludes useful control in this way.
No parasites
O
C£
O
Fusarium wilt only
^rsj
Botrytis crown rot only
Fusarium and Botrytis
Fig. 36. Diagrams illustrating some of the
difficulties of preventing Fusarium wilt of China
aster in southern California by planting in the
cool winter season. The shaded areas show the
soil temperatures that result in best growth be-
cause there is least damage from the indicated
diseases. Each disease restricts the range of
temperatures at which the crop can be grown.
40 50 60 70 80 90
SOIL TEMPERATURE ( F)
[50]
Makes possible the evaluation
of cultural practices
A diseased plant cannot grow as well
as its environment permits. This may be,
for example, because a deficient root
system restricts absorption, a deficient
leaf area reduces carbohydrate forma-
tion, or because an injured stem impedes
movement of water, nutrients, and foods
between them. For these reasons, a dis-
eased plant gives little indication of the
growth potentiality of its performance if
it were healthy. The only true indicator
of the value of any given cultural practice
is provided by a healthy plant with a
sound root system (Sec. 5).
Plants with defective roots may show
responses to fertilizer application rang-
ing from none to nearly normal, depend-
ing on the degree of root damage. Fer-
tilizer trials with plants of this nature
usually show no gains, whereas healthy
plants would have benefited from them.
It is difficult, therefore, for a grower to
determine, through experience, the best
fertilizer procedure for a crop unless he
deals with reasonably healthy plants.
Similarly, nutritional investigations
that use infested stock (even though it
appears clean), untreated soil, or both,
may provide no valid indication of the
potential response of the crop. Nutri-
tional research should be conducted with
healthy plants in order to be generally
applicable.
It is not necessary for a large part of
the root system to be injured to produce
serious effects. Plants sometimes show
severe injury from the mere loss of the
young white root tips, sometimes re-
ferred to by growers as loss of "root
action." This is because most of the ab-
sorption occurs in that zone of the roots.
Furthermore, the combining of the nitro-
gen absorbed by the roots, and the carbo-
hydrates formed by the leaves, into
amino acids may occur in the roots.
These acids are later used in forming the
proteins of the plant. Perhaps growth-
regulating substances are also formed in
the roots (Jackson, 1956). The whole
plant is thus seriously affected by partial
loss of roots.
If studies on irrigation practices are
conducted with plants that have diseased
roots, an entirely erroneous idea of the
water requirements of the crop will be
obtained. Furthermore, plants with in-
jured roots may wilt when exposed to
light of an intensity necessary for ade-
quate carbohydrate formation in the
leaves. If there is insufficient carbohy-
drate formed and conducted to the roots
they will be further weakened. Light re-
quirements may also be determined only
on healthy plants.
Reduces cost of
other disease controls
The use of disease-free stock fre-
quently reduces the cost of other disease-
control procedures. Thus, a California
celery grower found that seedlings grown
from hot-water-treated seed in steamed
soil were free from late blight, and when
planted in the field required spraying
only toward the end of the season, where-
as plants grown from untreated seed had
to be sprayed throughout the season.
Reduces danger of
disease panics
Periodic disease panics, such as those
concerning rose mosaic in 1929-1932
and chrysanthemum virus stunt in 1947-
1950, would be considerably reduced if
disease-free stock were more generally
used. Knowledge is the best defense
against these disturbing upheavals, par-
ticularly when it is put into practical use.
For additional benefits see sections 2
and 16.
[51]
SECTION
The Salinity Problem
in Nurseries
Warren R. Schoonover
R. H. Sciaroni
How the problem of salinity arises
Salt injury to ornamental plants
Detection of salts in the soil moisture
What can be done about salinity
The U.C.-type soil mixes and the salinity problem
R
Iurserymen are increasingly aware
of the fact that excess soluble salts in the
root zone have been responsible for the
failures of many ornamental and horti-
cultural plants. Excess soluble salts in the
soil, known as salinity, are not confined
to nurseries, but are quite common in
soils of arid and semi-arid regions.
Studies of the salinity problem with agri-
cultural crops in the laboratory and field
have yielded much information that is
directly applicable to the solution of the
problem in nurseries. This section has
been prepared so that growers will have
a better understanding of the salinity
problem and what can be done about it.
What are salts?
Salts are chemical compounds consist-
ing of an acid part, or ion, and a basic
part, or ion. For example, common table
salt — sodium chloride — consists of one
acid-forming ion, chloride, and one basic
ion, sodium. The two combine in chemi-
cally equivalent quantities to form a
neutral salt. Some common acidic ions
are sulfate, nitrate, phosphate, and bi-
carbonate. Common basic ions are cal-
cium, magnesium, potassium, sodium,
and ammonium. Any basic ion may com-
bine with any acidic ion, a great variety
of salts thus being formed.
HOW THE PROBLEM OF SALINITY ARISES
All nutrients needed for plant growth
arc; absorbed by the plants in the form
of salts or their ions. Some salts contain
no plant nutrients, others contain nu-
trients essential to the plants, and are
Ix-ncficial in proper amounts. All salts,
however, are harmful beyond the small
quantity needed for growth. The prob-
lem arises when the concentration of
soluble salts in the soil moisture reaches
levels that are harmful. Salts may come
from fertilizers, water, or soil.
[52]
Excess chemical and
organic fertilizers
In nursery soils the origin of harmful
salts is most frequently from chemical
and organic fertilizers which have been
used in excess (fig. 40). Chemical fer-
tilizers such as ammonium sulfate, am-
monium nitrate, and potassium sulfate
are already in the form of salts soluble
in water. Organic materials such as dried
blood, hoof and horn meal, and leaf mold
become mineralized through decay
processes, and the nutrients are finally
converted into salts. Nitrogen in the
organic form (for example, in hoof and
horn meal, manure, and leaf mold)
breaks down slowly under cool condi-
tions (Sec. 7). Growers may add such
a fertilizer, and when it does not become
available, add some quickly available in-
organic nitrogen. With return of warm
weather, accelerated decay processes may
produce a sudden excess of water-soluble
nitrogenous compounds which will cause
salinity injury.
Improper irrigation practices
Irrigation without proper attention to
leaching may cause a build-up of salts in
the root zone. Practically all irrigation
waters contain salts, sometimes in in-
jurious amounts (fig. 38). This accumu-
lation, added to that from fertilizers, may
result , in dangerous levels if periodic
leaching is not practiced. Injury is ag-
gravated by permitting a saline soil to
become somewhat dry (fig. 44). There
is evidence that salinity injury may occur
on some plants, such as begonias, from
the sprinkling of saline water directly on
the foliage (fig. 39). In addition, steam
and chemical soil sterilization may bring
about the release of certain chemicals,
such as ammonium, at levels toxic to
plants; this topic is discussed further in
sees. 6, 7, and 14.
Poor drainage and
soils initially high in salts
The use of soils with poor drainage,
especially those which already have a
high content of soluble salts (fig. 37) is
hazardous. Poor drainage restricts leach-
ing and may therefore lead to salt ac-
cumulation.
On several occasions serious financial
losses have been incurred when soils,
sedge peat, leaf mold, compost, manure,
and similar materials, high in content of
soluble salts, were used in growing mix-
tures. Some animal manures may be
particularly dangerous. In most feedlots,
manure is scraped up, dried, and sold.
Many feedlots use salt-grain mixtures to
fatten livestock. This salt, added to the
urine accumulated in surface manure by
the evaporation of water, may result in
extremely high salinity levels (figs. 41
and 42). During the past few years
nurserymen have been shifting towards
a standard soil mix such as the U. C.
type. One of the reasons for this shift has
been the danger involved in using many
unreliable ingredients in a soil mix, some
of which might be initially high in salts.
Clay pots and salt injury
It has been observed that used clay
pots may also contribute to the salinity
problem. This is because moisture
evaporation on the outside surface leaves
behind the soluble minerals in concen-
trated form (fig. 45). Roots which come
in contact with the pot may be injured
and even killed. It has also been shown
that soluble salts may cause rotting of
leaves of Saintpaulia which come in con-
tact with the salt crust on the rims of clay
pots. These problems may be avoided
by soaking the pots in water before using
them again (Sec. 12). They may be
eliminated by using cans or plastic con-
tainers.
[53]
37
40
38
41
-£:£<V&
39
42
SOURCES OF SALINITY
Fig. 37. Salts in the soil itself, many of them used by plants. Water moves to the surface carry-
ing salts, and evaporates, depositing them on the surface. Fig. 38. The water supply is a common
source of salts in California, from which they accumulate in the soil. Fig. 39. Drops of irrigation
water evaporate on leaves, leaving a salt deposit which causes local injury to some ornamentals.
Fig. 40. Fertilizer applications are important sources of salts added to the soil. They are usually
placed near the crown of the plant and the dissolved salts are then in the root zone. Fig. 41.
Animal manures from feed lots often carry large quantities of salts. Feed lots are often located
in saline depressions. The salts from the soil deposits and from urine accumulate in the surface
manure because of water evaporation there. Periodically the manure is scraped up, dried, and
sold. Leaf mold may have similar dangerous accumulations of salts. Fig. 42. Application of
animal manures or leaf mold to nursery plants often introduces injurious salts to the root zone.
(Based on a chart by K. F. Baker.)
I r>4 ]
SALT INJURY TO ORNAMENTAL PLANTS
Salinity injury occurs over a con-
tinuous range extending from no ap-
parent damage to rapid death. In the
lower concentrations of salinity there
may simply be reduced growth without
any visible symptoms. With somewhat
higher concentrations, the plant may
absorb considerable quantities of salt,
which tend to accumulate at the leaf
margins or tips and there will cause
actual burning when, through evapora-
tion, the concentration finally reaches a
lethal point (figs. 3, 46, 54, and 55). Of
course, this slow attrition may, with sus-
ceptible soft-leaved plants or plants
grown under full sun and under dry con-
ditions, lead eventually to death of the
plant. The more usual thing, however, is
to render it unproductive and unsightly
(figs. 53 and 58). If a plant is trans-
planted into a sufficiently saline soil, it
may collapse within a matter of hours.
There is a great variation among types
of plants as to salt tolerance. Some plants
(carnation) will tolerate fairly high
concentrations of soluble salts in the soil
moisture. The only symptoms may be a
slight yellowing and slow decline in
vigor. In contrast, some plants (gar-
denia) are so sensitive that root corro-
sion and scorching of the leaves will
develop shortly after exposure (figs. 56
and 57) .
Some saline conditions may cause con-
siderable injury to the roots (fig. 56).
Root injury due to salinity may lead to
chlorosis of foliage. Salinity injury to
the foliage of plants is accentuated under
conditions causing high transpiration
water loss; for example, in bright sun-
light under hot, dry conditions as op-
posed to humid, cool conditions. Shad-
ing greenhouses and humidifying the
atmosphere reduces transpiration and
hence the rate at which salt injury to the
foliage occurs (fig. 51).
Salinity may aggravate the losses from
seedling damping-off (Sec. 3). With
stocks in field plantings, salts accumulat-
ing in the tips of leaves may increase the
severity of attack by the Botrytis gray
mold (fig. 3, C) . Nematodes and fungi
may produce plant symptoms easily con-
fused with salinity injury.
In general, certain symptoms are
typical of the injury caused by excess
soluble salts. All or part of the following
may develop under conditions of high
salinity in the soil moisture.
Poor Germination of Seeds
Poor germination is particularly im-
portant in the growing of bedding plants
started from seed. Salts may build up
(fig. 43) to a point where germination is
greatly reduced. Seeds that do germinate
may produce plants that are stunted and
may be killed suddenly.
Many times the surface 1/4- to 1-inch
layer of soil may accumulate more
soluble salts than the second or third
inch. This situation may develop as a re-
sult of overfertilizing or insufficient
watering to induce leaching, or both.
Evaporation from the surface of the soil
will leave salts behind in a concentrated
form (fig. 43) . Therefore, the entire root
systems of small seedlings may be ex-
posed to high salt levels. When the sur-
face of the soil is allowed to dry slightly,
the concentration of salts in the soil
moisture increases and the seedlings die
quickly (compare figs. 43 and 44).
Injury to Tops and Roots
of Plants
Plants grown in containers or in raised
or ground benches under highly saline
conditions may develop all or part of the
following symptoms: plant stunting (fig.
53),. yellowing, wilting, or shedding of
leaves (figs. 57 and 58), tip or marginal
[55]
43 • ' ■
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~-»
45
ACCUMULATION AND CONCENTRATION OF SALTS
Fig. 43. Salts concentrate in soil surface from evaporation of water there, leaving a deposit
of salts in upper layers. This is the zone in which seeds germinate, and in which roots of seed-
lings and shallow-rooted annuals develop. Fig. 44. Salts become concentrated in soil when the
water content reaches low levels. Plant injury from salinity is thus aggravated by the practice
of "growing plants dry." Fig. 45. Salts accumulate in clay pots because water evaporates from
the surface, leaving a crust of salts. With many soils the roots are most abundant next to the
pot, exposed to saline conditions. Metal or other nonporous containers may be preferable in
California. Fig. 46. Salts accumulate in leaves, particularly at margins and tips, because water
evaporates from them, leaving salt accumulation behind. When these reach toxic levels the
tissue may be killed. (Based on a chart by K. F. Baker.)
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49 . ': .
PREVENTION OF SALINITY
Fig. 47. Rainfall or irrigation with deionized water will wash the salts down or (in containers)
leach them from the soil. Because no other salts are introduced, this treatment is very effective.
Fig. 48. Leaching soil with water of the best quality available, washes the salts from the bottom
of containers. The poorer the water used in irrigation, the greater the excess over plant require-
ments that must be used, and the more frequently leaching must be done. Fig. 49. Keep the
soil moist so that the salts are diluted and plant injury minimized. Fig. 50. Provide good drain-
age so that salts may be washed away. Keep holes open in pots and cans, and the bottom
cracks in benches; avoid hardpan soils. With poor drainage and high water table, salts remain
in place and concentrate from surface evaporation. Fig. 51 . Provide shade and high humidity
for salinity-sensitive plants, to reduce water loss from leaves and salt accumulation therein.
Fig. 52. Use fertilizers in small quantities as often as needed, interspersed with liberal watering.
This will keep salts at a low concentration. (Based on a chart by K. F. Baker).
[57]
\
Fig. 53. Soluble-salt in-
jury to camellia. The plant
on the left is healthy; the
one on the right was grown
under conditions where
soluble salts accumulated.
Symptoms were wilting and
severe leaf burn in some
cases.
"~*tm.£
m
Fig. 54. Salinity injury to Roosevelt fern. Note the marginal leaf burn on the left caused by
excess soluble salts in raised benches. Healthy leaf at right.
leaf burn (figs. 3, 46, 54, and 55), de-
creased root activity and sloughing of
roots (fig. 56), and complete collapse of
the top of the plant (fig. 57).
Experience with ornamentals has
shown that they react variously to excess
soluble salts. The symptoms described
below were observed under actual grow-
ing conditions in commercial nurseries.
Carnation, stock,
and amaryllis . . .
will tolerate relatively saline conditions.
A ^li^rht yellowing, particularly of older
leaves, and slow decline in \ Igor are typi-
cal. Production drops off slowly as salt
content increases.
Camellia, rhododendron, and
Roosevelt and Boston ferns
Tip or marginal burning of leaves de-
velops (figs. 54 and 55). There is also
decreased root activity and partial de-
foliation (fig. 53). When conditions
which have contributed to excess soluble
salts are removed, recovery may be very
slow. By the time the tops show visible
symptoms, considerable damage has al-
ready been done to the root systems.
I 58 1
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Fig. 55. Individual leaflets from Roosevelt fern, showing salinity damage. The two leaflets on
the left are healthy; the others show various stages of leaf scorch.
Fig. 56. Decreased root growth of gardenia caused by salt build-up resulting from too much
chemical fertilizer. The root system at the right is normal.
Fig. 57. Excess soluble salts caused wilting and collapse of tops of the three gardenia plants
at the left. The healthy plant at the right was grown under conditions of low salinity.
Fig. 58. The azalea plant on the left was killed by excess soluble salts. Poor drainage and
lack of aeration may cause similar symptoms on azaleas. The plant on the right is healthy.
Cymbidium orchids . . .
show a leaf tipburn and dieback. Cattleya
types become yellow, and new growth is
stunted.
Gardenia and azalea
Decreased root activity and sloughing
off of roots occur. There may be wilting
of leaves and sometimes a spectacular
collapse of the entire top of the plant
(figs. 56, 57, and 58). Excess salts are
often blamed for these conditions on
gardenia and azalea, however, when ac-
tually poor drainage and lack of aeration
are the real culprits. Azaleas have a high
requirement for good aeration and
drainage.
DETECTION OF SALTS IN THE SOIL MOISTURE
The Agricultural Extension Service,
commercial soil-testing laboratories, and
many growers are using instruments
called Wheatstone bridges to study sa-
linity problems. Salt solutions conduct
electricity to an extent approximately
proportional to the concentration, and
this conductance may be measured by
such bridges. Simplified forms of these
instruments called "Solubridges" are
available on the market. Two types are
in common use, the RD-26 and RD-15.
They measure electrical conductivity in
terms of reciprocal-ohms or mhos/cm.
Since the mho/cm is a large unit, a scale
reading in the range of salinity injurious
to plants would be expressed as small
decimals. Therefore, the units have been
divided by 1,000 into units called mil-
limhos or by 100,000 into unnamed
i<>0]
units. The scale on the Solubridge RD-26
gives readings in millimhos. Readings
obtained on the RD-15 Solubridge can
be converted to millimhos by dividing
by 100.
The U. S. Regional Salinity Labora-
tory, and the Agricultural Extension
Service and the Department of Soils and
Plant Nutrition, University of Califor-
nia, have adopted the saturated-soil-ex-
tract method for determining the salinity
of soils. An approximate value for the
concentration of soluble salts in the
saturation extract expressed as parts per
million (ppm) can be obtained by mul-
tiplying the reading on the RD-26 by
about 650, and the RD-15 by about 6.5.
Brief instructions for making soil-
salinity measurements using the extracts
from saturated soils are given on p.
62. Detailed directions can be obtained
from U. S. Department of Agriculture
Handbook 60 or the offices of the Agri-
cultural Extension Service. When exam-
ining soils and potting mixtures, it is
very important that the extract on which
the salinity measurement is made should
be directly related to the soil solution
which is actually in contact with the
roots. The best procedure would be to
extract some of the moisture with its dis-
solved salts from the moist soil in the
root zone of plants. Unfortunately, this
is too difficult to be practical. The next
best procedure is to saturate a soil
sample with distilled, salt-free water and
then take out some of the water by suc-
tion. This is easily done. The amount
of water required to saturate a soil is
directly related to the amount it will
hold under natural conditions of good
drainage.
If larger amounts of water are used,
such as 2 parts or 5 parts of water to 1
of soil, there will be no fixed relation
between the concentration in the extract
and the concentration in the soil solu-
tion. The results will be meaningless
when comparing one soil with another,
unless water-holding capacity is con-
sidered. For example, two greenhouse
soils containing equal amounts of solu-
ble salts were examined. No. 1 was a
sandy soil which would hold 24 per cent
water when saturated; no. 2 was a finer-
textured soil holding 64 per cent water
when saturated. Saturation extracts both
contained about 6,000 ppm of total salts,
a harmful amount, and gave conduc-
tivity readings of about 8 millimhos/cm.
When a suspension of 1 part of soil to
2 parts of water was examined, the first
soil gave a reading of 1.0 millimho/cm
and the second 4.5. By ordinary stand-
ards, the first soil would have been con-
sidered safe and the second quite in-
jurious. Both were actually salty to the
point that tender plants would have been
damaged severely.
Unfortunately, many laboratories still
report results on soil extracts of varying
soil/water ratios without including any
data from which one might predict
the probable salinity to which plant roots
are exposed. If growers use the satura-
tion-extract method it will be easier to
interpret their results, and all work done
will contribute to a common pool of
knowledge.
With agricultural crops in field soils,
it is pretty well known how much total
salinity can be tolerated and still secure
reasonable yields. This is not yet the
case with many ornamental and flower
plants. Additional experience is needed
with ornamentals, but experience to date
indicates that little or no difficulty will
be encountered if the concentration of
the saturation extract is around 2 mil-
limhos/cm. A concentration somewhat
lower than this will allow for ample
quantities of nutrient salts.
[61]
Procedure for Determining Salinity
by Saturation Extract Method1
1. Collect a soil sample which is representa-
tive of the root zone.
2. Prepare a saturated soil paste as follows:
Fill a pint container half full of the sample to
be tested. Add distilled water slowly until the
whole soil mass appears wet. Mix thoroughly
with a small stiff spatula or the handle of a
spoon, adding more water or more soil as may
be needed to reach the saturation point. When
this point is reached, the soil paste should
show the following characteristics:
A. Will be somewhat plastic and will tend
to shift or flow slightly when the con-
tainer is tipped.
B. Will slide freely from the spatula or
spoon, except in the case of a heavy
clay soil (may not be true of mixes
containing a very high percentage of
peat) .
C. Will show a very little free water in
surface depressions upon standing a
few minutes.
1 Adapted from methods in "Diagnosis and
improvement of saline and alkali soils," U. S.
Dept. Agr., Agr. Handbook 60, 1952.
When the saturation point apparently has
been reached, allow the sample to stand 15
minutes or longer, then restir, and recheck it
according to the three criteria above.
3. Remove an extract from this saturated soil
as follows: Set up a suction filtering assembly
(fig. 59; equipment listed in Appendix). A
convenient assembly consists of a size 1-A or
size 2 Biichner funnel fitted by a rubber stopper
onto a 500-ml side-neck suction (Erlenmeyer)
flask. It is advisable to catch the extract in a
test tube, 25 by 150 mm size, placed within the
flask. Vacuum is provided by connecting the
side neck of the flask to a filter pump. Place a
dry 7-cm hard (Whatman No. 50) filter paper
in the clean, dry Biichner funnel and fill with
the saturated soil paste. Apply suction and con-
tinue until enough filtrate is obtained to de-
termine conductivity. This determination will
require about 6 milliliters for rinsing a small
conductivity cell and making the test. This
amount of extract would fill the test tube de-
scribed to a depth of about 1 inch. Do not
continue suction after the soil dries and cracks,
and air starts passing through.
4. Determine electrical conductivity of the sat-
uration extract. The conductivity measurement
should be made according to the directions
furnished with the instrument you are using.
Fig. 59. A suction filtering assembly for making extracts of saturated soils. A Solubridge is
at the left. A filter pump, connected to a water faucet, provides a vacuum to speed the filtering
operation.
!
\p»«-.:
If the reading is in terms other than millimhos/
cm, convert to these units by shifting the
decimal point. The shift most commonly re-
quired is two places to the left, to convert from
the common unit EC x 105. The conductivity
cells with which tests are made are not always
accurately adjusted to give direct readings.
They can be tested with N potassium chloride
solution (see Appendix), which should give a
reading of 1.41 millimhos/cm. The amount of
the reading above or below this figure should
be added to or subtracted from the normal
setting for the observed temperature in each
case. It is important to test the solution at the
exact temperature for which the instrument is
designed, or to make a temperature adjust-
ment. Many instruments provide a dial for ad-
justing the temperature.
Test the extract you have prepared, as fol-
lows: If enough extract is available, rinse the
cell twice, discard the rinsings, and fill the
cell, being sure there are no air bubbles. If in-
sufficient extract is available for rinsing, wa<h
the cell out with distilled water, rinse it twice
with acetone, and take air in and out of the
cell until it is dry. Record the electric con-
ductivity reading in millimhos/cm.
WHAT CAN BE DONE ABOUT SALINITY
The problem of excess soluble salts
need not be troublesome to nurserymen.
Dangers of salt accumulations can be
minimized and practically eliminated if
proper practices are followed.
Water Quality and Proper
Irrigation Practices
The use of proper irrigation practices
is important in reducing the dangers of
excess soluble salt accumulation. In any
type of irrigated agriculture, nursery
stock included, it is always necessary to
use excess water to bring about some
leaching (fig. 48). In many nurseries,
constant water level and subirrigation
practices are used. With subirrigation,
salts accumulate on the surface of the
soil. One must be careful either to avoid
mixing these salts with the deeper soil, or
better yet, wash them down completely
through the bed by an occasional very
heavy watering. A light watering may
merely take these salt accumulations
down into the root zone where they will
cause great damage. Large amounts of
water will be required for these heavy
leachings if salts are allowed to build up.
In areas subject to salinity troubles, sub-
irrigation may be a dangerous method
for use by inexperienced operators.
Irrigation water should be low in salts
(fig. 47) . The Solubridge can be used to
measure the conductivity of water and
thus provide a measure of total salts in
water. A good water should give a read-
ing less than 1 millimho/cm, and should
have the individual constituents present
in favorable proportions. The conduc-
tivity, however, is only one of several
factors used in evaluating the quality of
irrigation water. It will be advisable to
have water from unknown sources, such
as wells, analyzed before planning exten-
sive use. When judging waters on the
basis of this item only, the higher the
conductivity the greater the amount of
water which must be leached through the
root zone. A water giving a reading of 2
or more would be relatively bad for most
ornamental plants even with satisfactory
ratios of the constituents. If used at all,
it should be applied in large quantities
to bring about leaching and prevent con-
centration.
Irrigation waters, in addition to the
danger of creating salinity problems in
the soil, may leave an objectionable
residue on the foliage of plants, usually
because of high calcium or magnesium
bicarbonate content (fig. 39). Several
large nurseries are using "deionizing
units" for removing all or part of the
salts from water. These units are expen-
sive initially but where a serious water-
quality problem exists, thev may prove
[63]
economical and practical in the long run.
Deionized water does not have to be re-
duced to the level of distilled water. It
can be blended with raw water to bring
down the total salinity. The use of "de-
ionizing units" or water sources already
low in bicarbonates will prevent water
spotting and therefore eliminate the
added expense of washing residue off the
leaves. Leaf absorption of salts is be-
coming more widely recognized. In
southern California a water moderately
high in sodium but containing practically
no calcium has defoliated azaleas under
conditions of sprinkler irrigation. Over-
head watering should be discontinued if
this situation is confronted.
The presence of high concentrations
of sodium offers a special problem in de-
termining water quality. If sodium is
high relative to calcium plus magnesium,
the water is likely to cause trouble. This
is especially true if the water is high in
bicarbonate rather than chloride or sul-
fate.
Another constituent which causes
trouble, even in concentrations as low as
0.5 ppm, is boron. Unfortunately, de-
ionizers do not remove boron.
If excess sodium or boron is suspected,
growers are urged to obtain a water
analysis. Every effort should be made to
develop a new source of irrigation water
if the analysis shows that the present
water is unsuitable.
The question often arises as to why
water -softening processes cannot be used
to remove salts from water for nursery
use. Waters are called "hard" when they
contain sufficient quantities of calcium
and magnesium salts to precipitate soap
to an undesirable extent. Common water-
softening processes do not remove salts
from the water, they merely substitute
sodium for equivalent quantities of cal-
cium and magnesium. This produces a
water which is more desirable for laun-
dry and washing purposes, but much less
satisfactory for irrigation.
Soils of moderate to high salinity
should be kept on the moist side to re-
duce plant injury (fig. 49) ; alternate
wet and dry conditions should be
avoided. Growing the plants under shady,
humid conditions also reduces water loss
from the leaves, and salt accumulation
in them (fig. 51).
Selection of Well-drained
Soils Low in Salts
It is a common practice for nursery-
men to use soil mixes in an effort to ob-
tain so-called well-drained growing
media. Drainage with sufficient leaching
is very important in a program to mini-
mize the salinity problem (fig. 50). No
pot or bed can be said to be really well-
drained, since the bottom layer must be-
come saturated before water will drip
into the air space beneath. A good
medium has good permeability, which
means that water will move quickly
through the soil to the lowermost zone
of saturation, from which it will drip.
The selection of a sandy soil, initially
low in total salts, such as is used in a
U. C. system, has proved practical and
efficient (sees. 5 and 6). Because of the
excellent permeability, the danger of ex-
cess soluble salt accumulation is elimi-
nated if the proper amount of fertilizers
is used. Further, with a U. C.-type mix
there is less danger of overwatering.
Proper Use of Fertilizers
Many nurserymen have gotten into
the habit of using more fertilizer than is
actually needed to produce adequate
plant growth and maximum quality (fig.
52) . This is perhaps due to the fact that
there is little concern over cost of ferti-
lizer for ornamentals, because of their
high value. Overfertilization has con-
tributed markedly to the problem of ex-
cess soluble salts.
Laboratory tests, field demonstrations,
and actual commercial usage have shown
that proper amounts of fertilizer applied
64
to a U. C.-type mix produce excellent
plant growth. All of this has been
achieved with practically no risk from
the danger of overfertilization and re-
sulting salinity problem.
The fertilizer schedules used in the
U. C. system would provide sufficient
plant nutrients with safety from the
standpoint of salinity (sees. 5, 6, and 7) .
Frequency of application of the fertilizer
will depend upon kind and size of plant,
amount of growth, container size, and
other factors. Conductivity readings of a
saturation extract from a U. C.-type mix
varies from 1.5 to 3.5 millimhos/cm.
This is considered a safe margin for most
ornamental plants, lower levels being
preferable for seedlings.
THE U. C.-TYPE SOIL MIXES AND THE SALINITY PROBLEM
The adoption of mixtures of fine sand
and organic matter as plant growing
media can help eliminate the salinity
problem because of increased perme-
ability and leachability of such mixtures.
In one of our experiments to determine
comparative leachability, potting mix-
tures were set up consisting of fine sand
alone, sand with 25 per cent and 50 per
cent peat, sand with 50 per cent fir bark,
loam with 50 per cent pine shavings,
loam with 50 per cent fir bark, loam with
50 per cent peat, and loam treated with
Krillium soil conditioner. All these
potting soils were salinized with a mix-
ture of sodium sulfate and calcium chlo-
ride to a salinity of approximately 7.0
millimhos/cm in the saturation extracts.
Leaching experiments were conducted to
study the rate of salt removal from soil
beds 1% inches in depth.
The results of these experiments are
diagrammed in figure 60. The vertical
scales indicate the electrical conductivity
of the leachate passing through the soil.
The horizontal scales indicate the depths
of water passed through the soil.
These experiments show (fig. 60, A)
that salts are removed rapidly from sand
and that the addition of organic matter
retards salt removal even though it may
improve permeability. The high initial
conductivity shows that much salt is re-
moved in the first portion of the leachate.
The less steep slopes for the mixes con-
taining peat indicate that the peat re-
tards salt removal. The lower initial con-
ductivity of the mix containing fir bark
indicates that the fir bark causes greater
salt retention than the peat. A total depth
of water (2 inches), which was greater
than the depth of the soil, was required
to reduce the salinity to reasonably low
levels.
Leaching with a dilute nutrient solu-
tion reduced the salinity, but a little more
slowly than leaching with tap water (fig.
60, B) . The nutrient solution seemed to
improve permeability of the sand and
permitted channeling around the organic
matter so that the first portion of the
leachate removed less salt from the mix-
tures containing 50 per cent of either
peat or fir bark. The addition of the
organic materials to loam evidently
caused channeling which permitted water
or nutrient solution to leach through the
soil without removing the salt. The flat-
ness of the curves in figure 60, C, D, E,
and F indicates that the salt is not being
removed in the first portions of the
leachate as with the sand mixtures. Tests
indicated that one third to one half of
the salt remained in these loam mixes
after about 2 inches of water had passed
through the 1%-inch layer of soil. The
Krillium did not improve the leacha-
bility.
It is evident that if there are sources
of salinity such as excess fertilizer or
poor-quality irrigation water, leaching
needs to be frequent and heavy to com-
[65]
Cond.
KxlO3
15-
14-
13-
12-
11-
10-
9-
8-
7-
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0-
Tap Water Leaching
Nutrient Solution Leaching
Fine Sand
x x Fine Sand + 25% Peat
e-—e Fine Sand + 50% Peat'
Fine Sand + 50%
Fir Bark
5-
4r
3-
2-
1-
0-
,-s.
Loam + 50% Fir Bark 1
&— e Loam + 50% Peat
*-o-
T 1
/
<^,
%
V*«L
^«^.
'■~o.
T 1
5-|
4-
3-
2-
1
0
_ Loam, Krilium Treated
_x Loam +50% Pine
Shavings
T
T
o'.5 l'.O 2.0 3.0
Inches Leachate
4.0
T
T
T
0.5 1.0 2.0 3.0
Inches Leachate
- 1
4.0
Fig. 60. Results of leaching experiments with U. C. and other soil mixes. The fine sand was
more easily leached than was the loam. Addition of organic materials retarded salt removal,
but peat did this less than the other forms tested. Nutrient solutions were less effective than
water in leaching. Conductance of the leachate is not a reliable index of salts remaining in
the soil.
[66]
bat the salinity problem. This is more
easily accomplished with fine-sand mix-
tures such as the U. C. type than with
those made from the finer-textured loam.
The results also indicate that measur-
ing the salinity of the leachate from a
pot or bed does not indicate how much
salt remains in the soil. Undesirable
quantities of salt may remain in soil after
the leachate has reached low levels of
salinity. Salinity should, therefore, be de-
termined from a soil sample. Heavy and
frequent leaching, if required, will neces-
sitate increased attention to supplies of
nutrients, particularly nitrogen.
The leachability of the U. C.-type
mixes makes possible the avoidance of
the salinity problem, but use of these
mixes is no insurance against salinity if
leaching is inadequate.
[67]
SECTION
The U.C-Type
Soil Mixes
Formulas for the soil mixes
O. A. Matkin
Philip A. Chandler
Application of fertilizers
Suggested uses of the U.C. soil mixes
Practical considerations
I
T is singular that so many problems
in nurseries arise from unsuitable grow-
ing media, when there are so many types
of them from which to select. Although
many excuses are offered for such
failures, the trouble usually lies in lack
of understanding of a few basic plant re-
quirements and methods of satisfying
them.
Since many soil mixes have already
been proposed and many successful
crops produced in them, it may seem un-
necessary to suggest another. Other sys-
tems or mixes, however, have failed par-
tially or wholly to satisfy the require-
ments, particularly that of reliability. If
a grower cannot depend on a certain soil
NOTE:
Copies of tables 1 through 8 are printed
in leaflet form for ready reference on
desk or wall. Ask your farm advisor for
Leaflet 89, "The U.C-Type Soil Mixes,"
or write to Agricultural Publications,
Room 22 Giannini Hall, University of
California, Berkeley 4, California.
mix to be similar in physical and chemi-
cal properties each time it is prepared,
he cannot plan his program of growing
with any degree of certainty, nor learn
from either his failures or his successes.
A system which provides complete physi-
cal and chemical reliability, along with
optimum conditions for plant growth,
should have world-wide value. The sys-
tem proposed is an attempt to satisfy
this need in the simplest manner pos-
sible.
The unique ingredient of the U. C-
type mix is fine sand. This material has
been avoided by research workers be-
cause it was considered too fine for sand
culture, and by growers and agricul-
turalists because of its low fertility. Sand
culture involves the use of coarse sand
or gravel with practically no moisture or
nutrient retention, these being continu-
ously supplied by nutrient solution. As
explained in Section 6, fine sand plus
peat approaches loam in water and nu-
trient retention, but avoids the compli-
cations involved where clay is present.
I 68 |
FORMULAS FOR THE SOIL MIXES
Physical Ingredients-
Basic Mix
-the
The ingredients of the basic mix are
fine sand and peat moss. The fine sand
must meet definite specifications; these
are given in Section 6. Canadian and Ger-
man sphagnum peat mosses and Cali-
fornia hypnum peat moss are satisfactory
for the organic ingredient, but many
black or sedge peats are not.
Although there are but two basic in-
gredients in the soil mix, by varying
their proportions a wide range of physi-
cal properties is obtainable. Five of these
variants are shown in table 1. Other ma-
terials, such as redwood sawdust or shav-
ings, or rice hulls may be substituted for
all or part of the peat moss, provided
they too satisfy the physical and chemical
requirements already mentioned and ex-
plained in more detail in Section 6. Pos-
sible variations within the basic prin-
ciple are therefore numerous.
Chemical Ingredients
Formulas for fertilizer addition to the
basic mix may also be quite numerous,
but they too follow a simple basic pat-
Table 1. The Five Basic U. C. Soil Mixes
Ingredients, per
cent by volume
Weight, pounds
per cubic foot
Maximum water
content f
pH with
fer-
tilizer
added
Approx.
cost per
cubic
yard
Soil
mix
Fine
sand
Peat
moss*
At max.
water
con-
tent f
Oven-
dry
Per
cent
by
volume
Per
cent
by
weight
Comments and suggested uses
A
100
0
117
89
43
30
7.0
$2.00
Seldom used; densest
and least retentive of
nutrients; for cans,
flats, beds
B
75
25
105
76
46
38
6.8
3.19
Commonly used ; good
physical properties ; for
cans, flats, beds
C
50
50
94
63
48
48
6.5
4.37
Commonly used; excel-
lent physical proper-
ties ; for pots and beds
D
25
75
66
34
51
94
6.0
5.56
Light weight, excellent
aeration; for pots and
beds
E
0
100*
43
7
59
530
5.7
$6.75
Very light weight; used
for azaleas, sometimes
gardenias and camel-
lias
* Redwood shavings may be used for part of the peat in mix E to improve aeration and reduce cost.
Redwood shavings or sawdust or rice hulls may also be used for some or all of the peat in other mixes.
f Maximum water content, and weight at that moisture level, are typical for a 6-inch column of a mixture
of fine sand of the Oakley series and Canadian peat moss.
[69]
tern. The fertilizer ingredients are nor-
mally added by weight to a volume of
physical mix. Mixing the physical in-
gredients and fertilizers can be carried
out in many ways. It is desirable to
establish accurately the volume of any
equipment used for measuring the physi-
cal ingredients. Uniformity of filling
measuring equipment with these in-
gredients is essential. This, with accurate
weighing of fertilizer additions, will in-
sure a consistent mix.
Typical variations of the fertilizer ad-
ditions suitable for the five examples of
basic mix for the U. C. system are given
in tables 2 through 6. Although these fer-
tilizer additions for the different mixes
correspond in general, each is adapted
to and should be used only with the mix
it is suggested for; thus fertilizer I (A)
should be used only with mix A, fertilizer
I (B) only with mix B, and so on.
A grower trying mixtures containing
hoof and horn should use several dif-
ferent rates to determine which is best
for his conditions of growing.
In the foregoing formulas lime has
been added in two forms, dolomite and
calcium carbonate, in order to bring the
pH up to a reasonable value and at the
same time supply proper proportions of
calcium and magnesium. If pH values
other than those listed are desired, the
lime additions may be altered to suit the
new requirements. Fine sand is fre-
quently found to be slightly acid in re-
action, though exceptions do occur. In
the event lime occurs in the fine sand
used, the lime additions may be reduced
in the mix.
Potassium nitrate is sometimes diffi-
cult to distribute uniformly in the mix
because it tends to cake. Many growers
rub the lumps over a window screen just
before mixing in order to reduce it to a
fine powder. Others dissolve the potas-
sium nitrate in water and sprinkle it into
the soil as it is being mixed.
Fertilizers used in small amounts are
sometimes difficult to mix uniformly in
the bulk ingredients. One of the best
methods of obtaining uniformity is to
mix all fertilizer components together
before adding the bulk ingredients. It
may even be helpful to mix some fine
sand with them during this premixing of
fertilizers.
As mentioned in Section 6, phosphate
may be added as either single or double
superphosphate. The formulas in tables
2 through 6 list single superphosphate.
If double is used, about one half as
much is required. One of the problems
in using the superphosphates is that
some grades are very coarse or in small
lumps, causing uneven distribution in
the mix. To overcome this the grower
should obtain a finely ground product.
If the best material obtainable is still
rather coarse, he might screen out the
lumps and then grind them to a powder.
Some growers have used technical-grade
monocalcium phosphate from chemical
supply houses in order to obtain a rela-
tively pure powdery product. The cost
of the technical-grade material is 2 to
3 times as high, but this is not a major
factor in the cost of the mix since mono-
calcium phosphate can be used at about
one third the rate of single superphos-
phate.
The amount of fertilizer added to the
basic mixes, is largely limited by the sa-
linity produced. The components which
contribute most to the salinity of the final
mix are potassium nitrate and potas-
sium sulfate. Of course, the breakdown
products of the organic nitrogen addition
will eventually also contribute to salin-
ity. The fertilizer additions listed above
will result in a saturation extract con-
ductivity of approximately 2.0 (Sec. 4).
The formulas are, therefore, a guide to
the amounts and types of materials that
may be safely added to any one of the
basic mixes. Numerous variations are
possible. A grower may wish to increase
or decrease the amount of any one of the
ingredients and observe the effect on his
particular crop. (Continued on p. 76)
[70]
Table 2. Chemical Ingredients for U. C. Soil Mix A
(100 Per Cent Fine Sand)
Use these fertilizers only with mix A
Amount of materials to be added to each cubic yard
These mixes may be stored indefinitely
Fertilizer I (A)
Fertilizer IV (A)
8 oz. potassium nitrate
12 oz. potassium sulfate
4 oz. potassium sulfate
23^ lb. single superphosphate
2^2 lb. single superphosphate
13^ lb. dolomite lime
. 1}^ lb. dolomite lime
2M lb. gypsum
23^ lb. gypsum
Contains moderate amount of
available
No available nitrogen included. Will re-
nitrogen but will require supplemental feed-
quire feeding as soon as planted. Good for
ing within a short time. Good
for rooted
holding plants back. Good for rooted cut-
cuttings and growing-on.
tings and growing-on.
Approximate cost 17 cents
Approximate cost 13 cents
These mixes should be planted
within one week of preparation
Fertilizer II (A)
Fertilizer V (A)
23^ lb. hoof and horn or blood meal
23^2 lb. hoof and horn or blood meal
8 oz. potassium nitrate
12 oz. potassium sulfate
4 oz. potassium sulfate
23^ lb. single superphosphate
2 ' j lb. single superphosphate
1J4 lb. dolomite lime
13^ lb. dolomite lime
2^ lb. gypsum
23^ lb. gypsum
Contains available nitrogen plus moderate
nitrogen reserve. Good for fast-growing
Moderate supply of reserve nitrogen with
rooted cuttings or transplants and liners.
none immediately available. Same uses as
Also used for potting-on.
formula II (A).
Approximate cost 35 cents
Approximate cost 31 cents
Fertilizer III (A)
Fertilizer VI (A)
5 lb. hoof and horn or blood meal
5 lb. hoof and horn or blood meal
8 oz. potassium nitrate
12 oz. potassium sulfate
4 oz. potassium sulfate
23^ lb. single superphosphate
1l/i lb. single superphosphate
1% lb. dolomite lime
\l/i lb. dolomite lime
2 3^ lb. gypsum
23^ lb. gypsum
Contains available nitrogen plus high nitro-
High nitrogen reserve with none immedi-
gen reserve. Good for potting-on where
ately available. Same uses as formula
plants are quite fast growing or where
III (A).
small amounts of soil are added.
Approximate cost 52 cents
Approximate cost 48 cents
[71]
Table 3. Chemical Ingredients for U. C. Soil Mix B
(75 Per Cent Fine Sand,
25 Per Cent Peat Moss)
Use these fertilizers only with mix B
Amount of materials to be
> added to each cubic yard
These mixes may be stored indefinitely
Fertilizer I (B)
Fertilizer IV (B)
6 oz. potassium nitrate
10 oz. potassium sulfate
4 oz. potassium sulfate
23^ lb. single superphosphate
2^2 lb. single superphosphate
43^ lb. dolomite lime
4^ lb. dolomite lime
134 lb. calcium carbonate lime
134 lb. calcium carbonate lime
134 lb. gypsum
134 lb. gypsum
Contains moderate amount of available
No available nitrogen included. Will re-
nitrogen but will require supplemental feed-
quire feeding as soon as planted. Good for
ing within a short time. Very good for
holding plants back. Same uses as formula
bedding plants and can growing.
KB).
Approximate cost 20 cents
Approximate cost 17 cents
These mixes should be planted
within one week of preparation
Fertilizer II (B)
Fertilizer V (B)
23^ lb. hoof and horn or blood meal
23^ lb. hoof and horn or blood meal
6 oz. potassium nitrate
10 oz. potassium sulfate
4 oz. potassium sulfate
23^ lb. single superphosphate
23^ lb. single superphosphate
43^ lb. dolomite lime
4.Y lb. dolomite lime
134 lb. calcium carbonate lime
134 lb. calcium carbonate lime
134 lb. gypsum
134 lb. gypsum
Contains available nitrogen plus moderate
Moderate supply of reserve nitrogen with
nitrogen reserve. Good for fast-growing
none immediately available. Same uses as
rooted cuttings, transplants, or liners. Also
formula II (B).
used for potting-on.
Approximate cost 38 cents
Approximate cost 35 cents
Fertilizer III (B)
Fertilizer VI (B)
5 lb. hoof and horn or blood meal
5 lb. hoof and horn or blood meal
6 oz. potassium nitrate
10 oz. potassium sulfate
4 oz. potassium sulfate
23^ lb. single superphosphate
23/> lb. single superphosphate
4'^ lb. dolomite lime
4 Yi lb. dolomite lime
134 lb. calcium carbonate lime
134 lb. calcium carbonate lime
134 lb. gypsum
134 lb. gypsum
Contains available nitrogen plus high nitro-
High nitrogen reserve with none immedi-
gen reserve. Good for potting-on where
ately available. Same uses as formula
plants are quite fast growing or where small
III (B).
amounts of added soil are used.
Approximate cost 55 cents
Approximate cost 52 cents
L72J
Table 4. Chemical Ingredients for U. C. Soil Mix C
(50 Per Cent Fine Sand, 50 Per Cent Peat Moss)
Use these fertilizers only with mix C
Amount of materials to be added to each cubic yard
These mixes may be stored indefinitely
Fertilizer I (C)
Fertilizer IV (C)
4 oz. potassium nitrate
8 oz. potassium sulfate
4 oz. potassium sulfate
23^2 lb. single superphosphate
23^ lb. single superphosphate
73^ lb. dolomite lime
73^ lb. dolomite lime
23^2 lb. calcium carbonate lime
23^2 lb. calcium carbonate lime
Contains moderate amount of available ni-
No available nitrogen included. Will re-
trogen but will require supplemental feed-
quire feeding as soon as planted. Good for
ing within a short time. Good for rooted
holding plants back. Same uses as formula
cuttings and growing-on. Easily rooted
1(C).
cuttings may be rooted and started in it.
Approximate cost 22 cents
Approximate cost 20 cents
These mixes should be planted
within one week of preparation
Fertilizer II (C)
Fertilizer V (C)
23^ lb. hoof and horn or blood meal
23^2 lb. hoof and horn or blood meal
4 oz. potassium nitrate
8 oz. potassium sulfate
4 oz. potassium sulfate
23^ lb. single superphosphate
23^ lb. single superphosphate
73^2 lb. dolomite lime
73^ lb. dolomite lime
23/2 lb. calcium carbonate lime
23^2 lb. calcium carbonate lime
Contains available nitrogen plus moderate
Moderate supply of reserve nitrogen with
nitrogen reserve. Excellent for greenhouse
none immediately available. Same uses as
pot plants, fast-growing rooted cuttings and
formula II (C).
liners. Very good for potting-on.
Approximate cost 40 cents
Approximate cost 38 cents
Fertilizer III (C)
Fertilizer VI (C)
5 lb. hoof and horn or blood meal
5 lb. hoof and horn or blood meal
4 oz. potassium nitrate
8 oz. potassium sulfate
4 oz. potassium sulfate
23^2 lb. single superphosphate
23/2 lb. single superphosphate
73/£ lb. dolomite lime
73^ lb. dolomite lime
23/£ lb. calcium carbonate lime
2}/2 lb. calcium carbonate lime
Contains available nitrogen plus high nitro-
High nitrogen reserve with none immedi-
gen reserve. Good for potting-on where
ately available. Same uses as formula
plants are quite fast growing or where small
III (C).
amounts of soil are used.
Approximate cost 57 cents
Approximate cost 55 cents
[73]
Table 5. Chemical Ingredients for U. C. Soil Mix D
(25 Per Cent Fine Sand, 75 Per Cent Peat Moss)
Use these fertilizers only with mix D
Amount of materials to be added to each cubic yard
These mixes may be stored indefinitely
Fertilizer I (D)
Fertilizer IV (D)
4 oz. potassium nitrate
8 oz. potassium sulfate
4 oz. potassium sulfate
2 lb. single superphosphate
2 lb. single superphosphate
5 lb. dolomite lime
5 lb. dolomite lime
4 lb. calcium carbonate lime
4 lb. calcium carbonate lime
Contains moderate amount of available ni-
No available nitrogen included. Will re-
trogen but will require supplemental feed-
quire feeding as soon as planted. Good for
ing within a short time. Good for
trans -
holding plants back. Same uses as formula
planting and for seed germination.
1(D).
Approximate cost 16 cents
Approximate cost 14 cents
These mixes should be planted within one week of preparation
Fertilizer II (D)
Fertilizer V (D)
2 ! ■_, lb. hoof and horn or blood meal
23^ lb. hoof and horn or blood meal
4 oz. potassium nitrate
8 oz. potassium sulfate
4 oz. potassium sulfate
2 lb. single superphosphate
2 lb. single superphosphate
5 lb. dolomite lime
5 lb. dolomite lime
4 lb. calcium carbonate lime
4 lb. calcium carbonate lime
Contains available nitrogen plus moderate
Moderate supply of reserve nitrogen with
nitrogen reserve. Very good for growing-on.
none immediately available. Same uses as
Reduced water requirement will enhance
formula II (D).
nitrogen efficiency, resulting in a lower
supplemental feeding requirement.
Approximate cost 34 cents
Approximate cost 32 cents
Fertilizer III (D)
Fertilizer VI (D)
5 lb. hoof and horn or blood meal
5 lb. hoof and horn or blood meal
4 oz. potassium nitrate
8 oz. potassium sulfate
4 oz. potassium sulfate
2 lb. single superphosphate
2 lb. single superphosphate
5 lb. dolomite lime
5 lb. dolomite lime
4 lb. calcium carbonate lime
4 lb. calcium carbonate lime
Contains available nitrogen plus high nitro-
High nitrogen reserve with none immedi-
gen reserve. Dangerous to use except for
ately available. Same uses as formula
very fast-growing crops owing to greater
III (D).
efficiency of nitrogen added.
Approximate cost 52 cents
Approximate cost 50 cents
[74]
Table 6. Chemical Ingredients for U. C. Soil Mix E
(1 00 Per Cent Peat Moss)
Use these fertilizers only with mix E
Amount of materials to be added to each cubic yard
These mixes may be stored indefinitely
Fertilizer I (E)
Fertilizer IV (E)
6 oz. potassium nitrate
6 oz. potassium sulfate
1 lb. single superphosphate
1 lb. single superphosphate
23^ lb. dolomite lime
23^ lb. dolomite lime
5 lb. calcium carbonate lime
5 lb. calcium carbonate lime
Contains moderate amount of available
No available nitrogen included. Will re-
nitrogen but will require supplemental feed-
quire feeding as soon as planted. Good for
ing within a short time. Good for starting
holding plants back. Same uses as formula
rooted cuttings and for potting-on and
1(E).
bedding.
Approximate cost 15 cents
Approximate cost 11 cents
These mixes should be planted within one week of preparation
Fertilizer II (E)
Fertilizer V (E)
23^ lb. hoof and horn or blood meal
23^ lb. hoof and horn or blood meal
6 oz. potassium nitrate
6 oz. potassium sulfate
1 lb. single superphosphate
1 lb. single superphosphate
23^ lb. dolomite lime
23^ lb. dolomite lime
5 lb. calcium carbonate lime
5 lb. calcium carbonate lime
Contains available nitrogen plus moderate
Moderate supply of reserve nitrogen with
nitrogen reserve. Nitrogen supply should be
none immediately available. Same uses as
sufficient for considerable period of time.
formula II (E).
Used for potting-on.
Approximate cost 33 cents
Approximate cost 29 cents
Fertilizer III (E)
Fertilizer VI (E)
5 lb. hoof and horn or blood meal
5 lb. hoof and horn or blood meal
6 oz. potassium nitrate
6 oz. potassium sulfate
1 lb. single superphosphate
1 lb. single superphosphate
23^ lb. dolomite lime
23^ lb. dolomite lime
5 lb. calcium carbonate lime
5 lb. calcium carbonate lime
Contains available nitrogen plus high ni-
High nitrogen reserve with none immedi-
trogen reserve. Nitrogen may be excessive
ately available. Same uses as formula
except where small amounts of mix are
m (E).
used in potting-on.
Approximate cost 50 cents
Approximate cost 46 cents
[75]
It would be desirable if investigators
and growers used the same system of soil
mixes so that information might be more
readily transmitted between them. For
example, the specific method used to pro-
duce blue hydrangeas, as opposed to
pink, can be followed by anyone using
the same reliable soil system. Here the
procedure might be to reduce or elimi-
nate superphosphate and lime, and to
add some aluminum sulfate.
If long-term crops are grown, or if
mixes containing little reserve fertilizer
are used, fertilizer supplement must be
added as either liquid or dry material
during the growing period.
APPLICATION OF FERTILIZERS
Dry Fertilizers liver the quantity of fertilizer desired
As much as possible it is desirable to into each container by some simple
use for dry-fertilizer application, ma- trigger mechanism. Suggested fertilizer
terials which are not readily soluble, in formulas and rates for containers are
order to avoid the danger of temporary given in tame i.
excess. Organic nitrogen and the super- Liquid Fertilizers
phosphates fall into this classification. r™ j . .1
£. r . r .,. ., there are numerous advantages in the
since most potassium iertihzers are avail- £ ■,. .j £ ..-.* T 1 • x
. , 1 - l 1 1 r 1 1 use 01 liquid iertilizers. Labor is tre-
acle only in soluble form, thev must be t1 j j 1 «.i_ x _«.«v ••
, n -i . 1 . aii ill quently reduced because the fertilizing
handled with caution. A slowly soluble , . i 1 1 • •
„ . , . J ., can be carried out during a normal lrri-
potassium irit has recently become avail- c 1 r . £ -r
r. , /c, r. ,, .11 .i 1 gation. such application is sate, it rea-
able (bee. 6). Materials that might be 11 : .. j a v
, , r 1. • sonable concentrations are used. Apphca-
used, and common rates 01 application .. - , j t
' p r 1 1 lif tions can be made at more trequent m-
per 1(JU square feet tor bed or bench ier- 1 • j • i
.... ^ . .. tervals in order to maintain nearly con-
tihzing are as follows: u 1 i r • -i u«i«* t'u
D stant levels ot nutrient availability, lhe
Hoof and horn meal 1 to 3 pounds disadvantage is that the nutrients added
Blood meal... 1 to 3 pounds ag R i(j are algQ more readn logt
Cottonseed meal 1 to 3 pounds , 1 i 1 • A 1 .,,
Castor pomace 1 to 3 pounds through leaching. Again, the possible
Fish meal 1 to 3 pounds combinations of materials are numerous.
Ammonium sulfate % to 1 pound Table 8 provides a simple set of all neces-
Calcium nitrate V2 to 1 pound sary variants providing the major ele-
Ammonium nitrate V^to1^ pound
Single superphosphate 2 to 4 pounds .
Double superphosphate 1 to 2 pounds lhe most commonly used liquid for-
Potassium sulfate V\ to 1 pound mulas are L-2 and L-7. Normal practice
Potassium chloride V± to 1 pound is to use the liquid fertilizer in place of
Potassium nitrate % to 1 pound a reguiar irrigation. These materials can
Potassium frit (Dura-K) 2 to 5 pounds , ,. , . , . . , ,P ■..
be applied without rinsing the toliage
Where containers are to be fertilized, afterward under all but extreme condi-
it is common practice to use spoon meas- tions of bright sunlight. Vegetable dyes
ures. These are available from any va- may be added to fertilizer concentrates
riety store in sizes ranging from % tea- as indicators of injection,
spoon up to I tablespoon. There is a Concentrates are more readily made
definite need for a more efficient dis- with hot water or by introducing steam
penser which could be adjusted to de- while dissolving. The solutions may be
I 76 I
Table 7. Supplementary Dry Fertilizers for Container-grown Plants
Suggested rates are for 6-inch pots, gallon cans, and beds or benches about
8 inches deep. Use proportionately more for larger, and less for smaller soil
volumes. The ingredients should be carefully mixed before application.
The rates suggested are substantial. If light watering is practiced, it may be
necessary to reduce the amounts used. Numerous combinations other than
those listed may be found useful by trial or soil testing. In the average sand-
peat mix the element required in greatest quantity is nitrogen, next is potas-
sium, and last is phosphorus.
SUPPLYING NITROGEN ONLY:
Fertilizer VII 1 heaping teaspoon
1 to 3 lb. per 100 sq. ft.
Hoof and horn or blood meal
Particularly useful for first applications to
plants in mixes with fertilizers I and IV, and
for extra nitrogen supplement in forcing.
SUPPLYING NITROGEN, PHOS-
PHORUS, AND POTASSIUM:
Fertilizer VIII 2 heaping teaspoons
2 to 5 lb. per 100 sq. ft.
4 lb. hoof and horn or blood meal
4 lb. single superphosphate
1 lb. potassium sulfate or chloride
May be required after plants have grown
for some time in the same container.
SUPPLYING NITROGEN AND
POTASSIUM:
Fertilizer IX 1 heaping teaspoon
1 to 3 lb. per 100 sq. ft.
6 lb. hoof and horn or blood meal
1 lb. potassium sulfate or chloride
Most useful in mixes A, B, and C, contain-
ing high proportions of sand, as these ele-
ments are most rapidly lost through leach-
ing.
SUPPLYING NITROGEN AND
PHOSPHORUS:
Fertilizer X 2 heaping teaspoons
2 to 5 lb. per 100 sq. ft.
1 lb. hoof and horn or blood meal
1 lb. single superphosphate
Most frequently used in mixes D and E
containing very high proportions of peat
moss, where the nature of the material re-
sults in most rapid removal of phosphate
from solution (phosphate fixation).
SUPPLYING PHOSPHORUS AND
POTASSIUM:
Fertilizer XI 1 heaping teaspoon
1 to 3 lb. per 100 sq. ft.
6 lb. single superphosphate
1 lb. potassium sulfate or chloride
Useful where plants are to be held back by
allowing nitrogen deficiency to occur. Well
suited to legumes.
[-!']
Table 8. Liquid Fertilizer Formulas for Use with U. C. Soil Mixes
Where an applicator is used, the liquid can be made up in concentrated form
and diluted through it to give the concentrations listed. A dilution ratio of
more than 1:200 is not practical as these solutions cannot be made much more
than 200 times as concentrated as listed. Solutions may be stored for extended
periods without deterioration.
Urea — 45 to 46 per cent nitrogen (may be dangerous to use if biuret is
present).
Ammonium nitrate — 33.5 per cent nitrogen.
Mono-ammonium phosphate (technical grade) — 12 per cent nitrogen, 61.5 per
cent phosphate (P O ).
Potassium chloride — 60 per cent potash (K..O).
Calcium nitrate — 15.5 per cent nitrogen.
Amounts per 100 gallons of water
SUPPLYING NITROGEN ONLY, EX-
CEPT FOR L-3 WHERE CALCIUM IS
ALSO SUPPLIED:
L-l: 1 lb. urea
L-2: 1 lb. ammonium nitrate
L-3 : 2 lb. calcium nitrate
Particularly useful for first applications to
plants in mixes with fertilizers I and IV,
and for extra nitrogen supplement in forc-
ing.
SUPPLYING NITROGEN AND POTAS-
SIUM:
L-8: 12 oz. urea
12 oz. potassium chloride
L-9: 12 oz. ammonium nitrate
12 oz. potassium chloride
Most useful in mixes A, B, and C containing
high proportions of sand, as these elements
are most rapidly lost through leaching.
SUPPLYING PRIMARILY PHOSPHO-
RUS AND POTASSIUM, BUT IN-
CLUDING A SMALL AMOUNT OF
NITROGEN:
L-10: 12 oz. mono-ammonium phosphate
12 oz. potassium chloride
Useful where plants are to be held back by
allowing nitrogen deficiency to occur. Well
suited to legumes.
SUPPLYING NITROGEN AND PHOS-
PHORUS:
L-4: 12 oz. urea
12 oz. mono-ammonium phosphate
L-5: 12 oz. ammonium nitrate
12 oz. mono-ammonium phosphate
Most frequently used in mixes D and E
containing very high proportions of peat
moss, where the nature of the material re-
sults in most rapid removal of phosphate
from solution (phosphate fixation).
SUPPLYING PRIMARILY PHOSPHO-
RUS, BUT INCLUDING A SMALL
AMOUNT OF NITROGEN:
L-ll: 1 lb. mono-ammonium phosphate
Useful when phosphate is low.
SUPPLYING NITROGEN, PHOSPHO-
RUS, AND POTASSIUM:
L-6: 8 oz. urea
8 oz. mono-ammonium phosphate
8 oz. potassium chloride
L-7: 8 oz. ammonium nitrate
8 oz. mono-ammonium phosphate
8 oz. potassium chloride
May be required after plants have grown
for some time in the same container.
SUPPLYING POTASSIUM ONLY:
L-12: 1 lb. potassium chloride
Useful when potassium is low.
[78]
stored for extended periods without de-
terioration. Examples of application of
these formulas are given below.
Biuret Injury
Many commercial ureas and urea-for-
maldehyde preparations have been found
to contain biuret, a chemical by-product
formed in the manufacture and prepara-
tion of these nitrogen fertilizers. Biuret
is toxic to most plants, the typical symp-
toms being stunting, leaf burn, chlorosis,
and even death of the plant. Unless the
manufacturer labels the bag or con-
tainer, the only means of determining
the biuret content of the urea fertilizer
is by analysis or biological test. Since
this toxic ingredient may be a serious
hazard in plant production, the grower is
advised to exercise extreme caution in
the use of fertilizers containing or de-
rived from urea. Unless labeled biuret-
free, these materials should be used only
after thorough testing on each crop.
SUGGESTED USES OF THE U. C. SOIL MIXES
The type of growing operation will
largely dictate the choice of soil prepara-
tion and handling. The following are
typical procedures for several types of
growing. It is assumed that in all cases
the soil mix will be steamed or fumigated
for weed and disease control prior to
planting.
When a single growing procedure is
altered it usually affects other operations,
and a general adjustment to new meth-
ods may be required. Adoption of U. C-
type soil mixes is no exception to this.
Watering procedures must usually be
modified for best results. Some growers
have found that, because of more rapid
crop growth, the production schedule is
altered. While planting dates may need
to be altered to accommodate schedules,
faster production will lower cost and in-
crease volume.
Flats
Mix B will be used for most bedding
plants with the possible exception of
some of the shade plants, such as be-
gonia and primula, where mix C might
be used. Seed flats will normally be of
the same soil preparation as growing
flats.
The appropriate fertilizer I, II, IV, or
V is added to the basic mix. Since some
[
danger from ammonium excess exists
where organic nitrogen is present in
quantity, many growers avoid this pos-
sibility by using fertilizer I or IV
throughout. If organic nitrogen is
omitted, fertilizer is normally applied
soon after transplanting. If fertilizer I is
used, application of subsequent material
is normally delayed 1 to 2 weeks, then a
broadcast application of blood or hoof
and horn meal may be made, or a pro-
gram of using liquid nitrogen as formula
L-2 or L-3 may be used at 1- to 2-week
intervals. If plants are held for an ex-
tended period, fertilizer VIII may be
used for broadcast application.
In a few words, one procedure would
be:
Physical mix B.
Fertilizer I (B) .
After 2 weeks use liquid L-2 at
10-day intervals on transplants. Use
no additional fertilizer on seed flats.
One week prior to sale of trans-
plants, apply fertilizer VIII at 4
pounds per 100 square feet of flat
area.
Pots
Pot plants may start with rooted cut-
tings planted in 2%- or 3-inch pots
with one or more subsequent shifts up-
79]
ward in pot size before the product is
ready to sell. Many variations are prac-
ticed. Some growers actually place the
rooted cuttings in 6-inch pots, carrying
them in these to salable size. By proper
selection of fertilizer formula this is both
possible and entirely practical, saving
considerable labor in transplanting. The
following suggestions, however, are in-
tended for the common transplanting
and shifting procedure.
Rooted cuttings will be placed in mix
C fortified with fertilizer I (C), II (C),
IV (C), or V (C). When well rooted in
the new medium, dry fertilizer might be
applied as fertilizer VII, or liquid L-l,
L-2, or L-3. When ready for shifting to
larger pots, the soil preparation will be
mix C or D, with the appropriate ferti-
lizer III or VI. If the plants are held for
a short period no further fertilization
should be required. If held for a. long
time, dry fertilizer VIII or a program of
liquid fertilization with liquid L-6 or
L-7 may be used.
In brief, one procedure might be:
Plant rooted cuttings in 2V2-incn
pots of mix C, fertilizer I (C).
After 10 days start using liquid
L-2 at 10-day intervals.
Shift 21X>-inch liners up to 6-inch
pots using physical mix D and fer-
tilizer III (D) . If plants are held for
more than 2 months in 6-inch pots,
apply 1 heaping tablespoon fertilizer
VIII to each.
Cans
In can-grown nursery stock the cost of
the soil preparation is a very important
factor, and in many cases the shipping
weight is also economically important.
For these reasons, nurserymen may use
materials in the physical mix which will
reduce both cost and weight of ingredi-
ents. Shavings, sawdust, bark, and even
rice hulls are currently in use as substi-
tutes for part of the peat moss. Nursery-
men should acquaint themselves with
these and other possibilities, keeping in
mind that any substitute material must
conform to the standards outlined in
Section 6 if reliability is to be retained.
For this type of growing, physical
mix B might well be used as the base,
with fertilizer I (B), II (B), IV (B), or
V (B). If soil is to be stored for any
length of time, as is frequently done, the
fertilizer formulas are limited to I (B)
or IV (B). The liners which are to be
planted into gallon cans may be handled
the same way as rooted cuttings under
the discussion of pot plants. If mix B
and fertilizer I (B) are used, either dry
fertilizer VII should be applied about 2
weeks after planting, or liquid L-2 or
L-3 should be applied at that time and
repeated at approximately 10-day in-
tervals. After plants are well established,
dry fertilizer VIII may be applied or the
liquid program shifted to liquid L-6 or
L-7. When plants in gallon cans are
moved up to egg cans (3-gallon size) or
5-gallon cans, the same procedure of fer-
tilizing may be carried out as was out-
lined for liners into gallon cans.
A typical procedure would be:
Grow liners as described for pot
plants.
Transplant liners into gallon cans
using mix B, fertilizer I (B).
After 2 weeks begin applications
of liquid L-2 every third irrigation.
After 2% months shift to liquid
L-7.
Just before plants are sold, or in
preparation for the winter rainy sea-
son (when liquid fertilizer cannot
be applied), use dry fertilizer VIII.
Benches and Beds
Plants grown in benches or beds
would include cut flowers as well as
stock plants from which cuttings are pe-
riodically taken.
Usually this type of growing is carried
out in the glasshouse, but in warmer
climates it may take place outdoors. The
inilial cost of bed preparation may be
80 ]
substantial, but when one considers the
potential useful period in terms of
seasons or years, it is obviously unwise
to economize on important ingredients.
Mix B may be satisfactory, but mix C
offers greater insurance of desirable
physical properties for optimum growth.
As discussed under "Cans," it may be
possible to substitute other organic mate-
rials for part of the mix, to provide the
best possible physical conditions at re-
duced cost. In commercial establish-
ments the U. C.-type soil mixes (25 per
cent or 50 per cent peat) have given good
lateral distribution of water applied to
the surface by the porous-hose or drip
system.
Beds might be prepared by using mix
C and fertilizer II (C) or V (C) if they
are to be planted at once. If planting is
to be delayed, fertilizer I (C) or IV (C)
should be used. If fertilizer II (C) or
V (C) is used, subsequent application
may begin 4 to 6 weeks after planting.
Regular applications of dry nitrogen
sources will be required for a few
months, and then it may be necessary to
use one of the mixed dry fertilizers from
time to time. Because of the length of the
growing period, it is impossible to out-
line a reliable long-term procedure here.
Liquids may be used in place of the dry
applications, keeping in mind that nitro-
gen will be required at first, with mixed
materials later. If fertilizer I (C) or
IV (C) is used, application should start
1 to 2 weeks after planting, with subse-
quent procedure the same as above.
An example might be as follows :
Prepare bed with mix C plus fer-
tilizer IV (C).
Apply starter solution as liquid
L-2.
Apply liquid L-2 every third irri-
gation for 6 weeks, then shift to
liquid L-7 every other irrigation.
When the beds are renewed or re-
planted more peat can be added.
[
Planter Boxes and Dish Gardens
Present-day landscaping makes com-
mon use of planter boxes both indoors
and outside. Standard soil mixes of the
types described are useful for a wide
range of plants. For large boxes with
adequate drainage use mix B or C, with
the appropriate fertilizer I, II, or V, fol-
lowed by the same feeding program as
for bench- or bed-grown crops. Dish
gardens or beds with obstructed drain-
age may use mix D or E with the appro-
priate fertilizer I, II, or V, but should
receive little or no subsequent fertilizing.
Home-Yard Planting
Where the natural soil is of a fine
sandy texture, a U. C.-type mix may
easily be prepared. Where the natural
soil is not of this type, an expensive
alternative is to remove and replace the
existing soil with the more desirable
kind.
When setting out plants grown in con-
tainers of fine sand and peat into soil of
different texture, an effort should be
made to blend the soil of the container
with the existing soil so that a transition
zone is produced. If proper planting pro-
cedures are followed, plants raised in the
fine sand and peat mixes will grow very
well even in heavy clay soils. The exten-
sive root systems produced in these
mixes favor more rapid establishment
when transplanted.
Frequently it is necessary in landscape
work to bring in top soil. The U. C.-type
mixes have proved successful, simple to
handle, and relatively inexpensive, par-
ticularly if cheaper organic materials
such as redwood sawdust or shavings, or
rice hulls are used in place of peat.
For Research
It is common practice in a research
glasshouse to steam or otherwise treat
soil for growing test plants, to protect
them from soil-borne diseases. The need
for healthy, vigorous, and uniform plants
81]
is obvious whatever phase of botanical
or agricultural science is under investi-
gation (p. 51). The importance of soil
in the production of experimental plants
is often underrated, and wholly unsuita-
ble soil types used. Poorly grown and ex-
ceedingly variable plants result.
The U. C.-type soil mix answers the
demands for growth of many kinds of
experimental plants. In studies of soil
pathogens it may be used (1) immedi-
ately after steaming, before it becomes
extensively recolonized, or (2) after the
soil has again developed a stable flora
from air contaminants, contact, or in-
oculation with a specific flora. For
routine tests of the pathogenicity of or-
ganisms on underground tissues, the
U. C.-type mix in such a biologically
buffered state provides conditions similar
to those in a natural fertile sandy loam.
When tests of pathogenicity and the
manifestation of symptoms demand
vigorously growing and uniform plants,
a U. C.-type soil mix is generally excel-
lent as a growing medium.
There are also examples of research
for which the desirable attributes of the
U. C.-type mix disqualify it. Thus it
would be unsuitable for studies on re-
sistance to a Phytophthora root rot
which normally occurs in a heavy, poorly
aerated soil. Wherever the qualities of
the soil itself constitute an important
factor in the problem under study, a
natural soil, or a soil mix with suitable
properties, should be given preference.
Apart from numerous uses in the study
of diseases induced by fungi, bacteria,
and nematodes, the U. C.-type mix has
proved to be excellent for growing plants
for virus research. In this field the re-
quirements for uniformity are often as
demanding as in the most accurate
physiological studies on soil-grown
plants.
Turkish tobacco plants have been
grown l>\ J. G. Bald and P. A. Chandler3
in 4-inch pots from seed to a height of
aboul L5 inches, bearing 15 to 18 ex-
panded leaves, within a period of 7
weeks from seeding. The average rate
of increase in leaf area in lots of 600
plants has reached 25 per cent per day.
From the emergence of the first true leaf
above the cotyledons until near the end
of this period the leaf-area growth rate
was logarithmic, provided greenhouse
conditions remained uniform. Percentage
increases in leaf area from day to day
were the same whether the plants were
small or relatively large. For much of
that time fresh weight of the tissues was
almost linearly related to leaf area ; later
the relation was more complex, but
regular and predictable. The logarithmic
growth rate was reduced by the crowd-
ing of roots in the 4-inch pots before the
physiological changes preceding flower-
ing could take effect. By growing herba-
ceous plants in larger containers of a
U. C.-type soil mix it should be possible,
for a particular set of conditions, to
maintain uniform and unrestricted
growth until seeding. It was possible with
this soil to transplant tobacco seedlings
in the cotyledon stage without loss, or
even a noticeable check to growth.
The physical characteristics are so
good that the first roots of the tiniest
seedling or of the largest plant pass
directly through the soil mass without
being diverted to the edge of the con-
tainer (fig. 61) .
In addition to rapid growth, experi-
mental plants in a U. C.-type mix, if
correctly selected and handled, exhibit
remarkably uniform size and habit.
There are several factors unrelated to the
soil mix which affect uniformity of plant
growth. Among them are: (1) heritable
variability between seedlings, even
within a horticultural variety; (2)
rapidity of seed germination; (3) dif-
ferences in extent of roots, caused in part
by development of recolonized non-
pathogenic organisms in any treated
soil; (4) other random sources of vari-
1 Department of Plant Pathology, University
of California, Los Angeles.
[82]
Fig. 61. Root development of Croft lily in U. C. mix C (50 per cent peat). Plant at left in the
soil ball, at right washed free of soil. Note the size of the root system and its development
throughout the ball.
ability. A group of plants grown in a
U. C.-type soil mix may superficially
appear more variable than those grown
in other soil because the more rapid
healthier growth accentuates the inherent
differences. For example, a plant arising
from a seed that germinated 3 days later
than its neighbors will appear relatively
smaller in a rapidly growing series than
it will in one of poor growth. Plants
grown under optimum conditions in a
soil mix of the U. C. type may be sorted,
accurately matched, and practically all
undesirable plants eliminated, with the
assurance that the maximum variability
is revealed. Such selected plants are
often comparable, leaf by leaf, from the
cotyledons to the growing tip, and they
will remain so through the period of the
experiment. On the other hand, poorly
grown plants cannot be matched in this
way. Their apparent similarity may mask
sources of variation that eliminate all
chance of obtaining accurate information
from experiments in which they are used.
The U. C. mixes will prove very useful
in the research greenhouse wherever
the production of uniform, well-grown
plants is desired for experimental studies.
The uniform growth rate may be main-
tained during the experiment if other
conditions are favorable.
PRACTICAL CONSIDERATIONS
Preparation of the Mixes
The mixing of the fine sand, peat or
other organic material, and fertilizer
components can be very simple. Peat
should be wetted before being mixed,
preferably 1 or 2 days before use. The
fine sand, peat or other organic material,
and the mixed fertilizers should be in
[83]
piles convenient to the mixing operation.
Complete mixing is essential.
If mixing is done by hand, the proper
amounts of the various ingredients
should be placed in a low, level pile with
the fertilizer components broadcast
evenly over the surface. This should be
turned with a shovel, progressively work-
ing through the mass from one side and
forming a second pile as the shovels of
soil are turned over. This second pile is
then turned back again, and the process
repeated until blending is complete.
If mixing is by machine, it is generally
done with a concrete mixer (Sec. 17) or
a ribbon mixer. In the smaller nursery a
small cement mixer may be used and
ingredients added by hand. In larger
operations, the major ingredients (fine
sand, peat) are generally placed in the
mixer with a skip loader and the fertilizer
components added by hand.
Moist, but not excessively wet, base
ingredients are essential to uniform mix-
ing and to reliability of subsequent treat-
ment.
Watering Practices
Since fine sands do not have cementing
properties (Sec. 6), the particles can be
readily dislodged. If heavy streams of
water are applied to fine sand and or-
ganic mixes, the surface is churned up,
and the sand settles first. The organic
matter therefore collects on the surface.
Where mulches are undesirable, it is
necessary to use water breakers during
irrigation to avoid this effect on U. C-
type mixes.
Some adjustment in watering prac-
tices is generally desirable when the
grower first uses a U. C.-type mix if he
has been accustomed to a clay soil.
Dump Soil
In any necessary operation a certain
amount of used soil is apt to accumulate.
This is probably more true of the bed-
ding-plant operation than of any other.
J. L. Mather" found that in 15 repre-
sentative California bedding-plant nur-
series an average of 16 per cent of the
flats were dumped. The problem of dis-
posal of this material sometimes assumes
major proportions. Since the physical
texture and structure of used U. C.-type
soil will be quite acceptable, the problem
is centered on its chemical properties. If
it is to be re-used, it is necessary to know
whether to add fertilizer, and if so, how
much.
For obvious reasons no standard pro-
cedure can be proposed which would
take into account all the possible varia-
tions which will exist. Several sugges-
tions, however, may be made:
1. Sell the material as top soil for
landscaping or similar use where
physical, rather than chemical,
properties are of prime importance.
2. Check the salinity of the soil by
the saturation-extract conductance
method (Sec. 4) and, if it is satis-
factorily low, use a portion of this
soil as a substitute for the fine sand
in the standard mix.
3. Determine by adequately complete
analysis the exact nutrient status of
the used soil, and calculate exactly
what to add in order to bring it up
to standard.
Cost of the Soil Mixes
Cost of a soil mix will be determined
by the cost of the soil, transportation to
the nursery, organic ingredients, ferti-
lizers, and labor in mixing. A major dif-
ference in cost between the older type of
composted mixes and those of the U. C.
type is that of labor. With a compost the
materials are handled at least 2 or 3
times before treatment, whereas mixes
of the U. C. type require only one opera-
tion.
There is also the lower cost of the
materials themselves. Fine sands will
8 Manager of the former Bedding Plant Ad-
visory Hoard, Bureau of Marketing, California
Stale Department of Agriculture.
[84]
usually be cheaper than top soil because
of the more efficient machinery that can
be used in digging the material, often to
a considerable depth. Top soil often is
more costly because only the surface
layer of limited areas is removed, using
less efficient machinery. In many areas
the price for top soil is greater than for
fine sand because of competition for it.
Soil-conservation practices also often
forbid the removal of top soil. Some of
the fine sands that are suitable for use in
U. C.-type mixes are actually waste
products from the screening and washing
of building materials.
Probably the main factor in any soil
cost will be the transportation charge.
Every nurseryman should try to locate a
source as close to his nursery as possible.
Assuming an average 33 per cent
shrinkage of leaf mold, manure, or other
compost materials, the cost per useful
unit volume should be increased by one
half over the purchase price. One cubic
foot of baled peat, on the other hand,
yields 1.5 to 1.6 cubic feet of loose
material.
Besides the lower labor requirement
mentioned above, comparative cost of
ingredients, mixes, and composts shows
that the U. C.-type mix is less expensive
than other common soil preparations.
Computed at 1955 wholesale prices, de-
livered to a near-by nursery in the Los
Angeles area, the cost per cubic yard of
some ingredients is as follows:
Fine sand S 2.00
Top soil $ 3.00
Peat moss, loose $ 6.75
($4.50 per 12 cu. ft. bale)
Sawdust $ 1.00
Leaf mold $13.50
($9.00 per cu. yd. delivered; 33 per cent
shrinkage sustained)
Steer manure $ 9.00
($6.00 per cu. yd. delivered; 33 per cent
shrinkage sustained)
Using these materials, the cost per
cubic yard of various nursery soil mix-
tures may be computed as shown in
table 9.
Table 9. Comparative Cost of Common Soil Mixes
Soil mix
STANDARD U. C. MIXES
A (100% fine sand)
B (75% fine sand, 25% peat)
C (50% fine sand, 50% peat)
D (25% fine sand, 75% peat)
E (100% peat)
U. C. MIXES USING SAWDUST
B (75% fine sand, 25% sawdust)
C (50% fine sand, 50% sawdust)
D (25% fine sand, 75% sawdust)
E (100% sawdust)
COMPOST
75% top soil, 25% leaf mold. . . .
50% top soil, 25% leaf mold,
25% manure
50% top soil, 50% leaf mold
100% leaf mold
Cost of ingredients per cubic yard of mix
Soil
$2.00
1.50
1.00
0.50
1.50
1.00
0.50
2.25
1.50
$1.50
Peat
$1.69
3.37
5.06
$6.75
Saw-
dust
$0.25
0.50
0.75
$1.00
Leaf
mold
$3.37
3.37
6.75
$13.50
Manure
$2.25
Total
$2.00
3.19
4.37
5.56
6.75
1.75
1.50
1.25
1.00
5.62
7.12
8.25
$13.50
[85]
SECTION
Components and
Development of Mixes
O. A. Matkin
Philip A. Chandler
Kenneth F. Baker
Functions of the soil
Disadvantages of multiple soil mixes
Attempts to improve nursery soil mixes
Soil toxicity in relation to treatments
Criteria for physical ingredients of soil mixes
Selecting ingredients for U.C. mixes
o
ne OF the commonest erroneous
ideas in nursery practice is that a special
soil, resembling as closely as possible the
soil of its native habitat, is required for
each type of plant. This involves the fal-
lacious assumption that distribution of
wild plants is determined by soil type,
whereas actually the temperature, rain-
fall, day length, light intensity, soil
salinity, the point of origin, as well as
other factors, are at least as important in
determining where plants grow. It may
actually be misleading to assume that the
best soil for a plant is that of its native
habitat, since the plant may have had to
"tolerate" that soil because another
factor, such as frost, may have limited it
to that particular area. Most plants of
necessity must have a wide tolerance to
soil types in order to survive.
The soil used may simply be a matter
of tradition. Some growers plant verbena
in straight leaf mold although it is not a
native of dense woodlands, and lilies in
black adobe although they require good
drainage. The surprisingly good results
sometimes obtained in such media testify
to the tolerance of plants in this regard.
The John Innes Horticultural Institu-
tion (Bayfordbury, Hertfordshire, Eng-
land) demonstrated in 1934-1939 that
many kinds of plants could be grown in
a single soil mix, or in slight modifica-
tions of it. As this concept has been
recognized by growers, there has been a
trend away from specialized mixes for
each type of plant.
FUNCTIONS OF THE SOIL
Any good growing medium must pro-
vide for the basic requirements of the
plants in it. Since all green plants have
the same basic requirements, the prob-
lem is simplified. The growing medium
supplies only the following functions.
[86]
Support
Most crops require some means of
physical support. Unless artificially pro-
vided, this is a function of the growing
medium; support is not a factor of major
concern unless the plant is large and the
growing medium of very light-weight
material such as peat moss. In nursery
growing it is common to use stakes and
ties of various types to support plants in
small containers.
Moisture
The living plant is largely composed
of water, which must be obtained from
the soil in which it grows. A good grow-
ing medium should have a reasonable
ability to hold moisture in sufficient
supply for plant requirements between
irrigations. Water is more often limiting
to plant growth than such items as ferti-
lizer, salinity, or alkalinity, which are so
often blamed.
High salinity (Sec. 4) may virtually
make soil water unavailable to the plant
because dissolved salts increase the os-
motic pressure in the soil solution. If the
concentrations outside the root approach
those within it, owing to dissolved salts,
water movement into the plant is re-
stricted.
Since containers have limited depth,
a boundary exists at the bottom in con-
trast to a continuous soil column in the
field. This boundary constitutes a restric-
tion to free drainage (Baver, 1956;
Huberty, 1945). Thus, soil in a con-
tainer will retain more moisture avail-
able to plants after an irrigation than it
would in the field.
Large quantities of water are lost by
the plant through transpiration; when
the plant wilts, this indicates that loss is
greater than the supply from the roots.
Although this is the major plant use of
water, it is bv no means the only im-
portant one. Water is the solvent in which
minerals are taken into and transported
through the plant. The two elements
comprising water, hydrogen and oxygen,
play individually important roles in plant
metabolism. All of the organic materials
of plants contain large quantities of each.
The fact that plants can be grown in
water (culture-solution growing) in-
dicates that there is no such thing as ex-
cessive water where the other basic re-
quirements are satisfactorily met. On the
other hand, plant growth unquestionably
can be restricted by conditions which
subject the plant to increasingly deficient
moisture. Frequently this point is over-
looked by the grower unless he happens
to have a comparison available. The ac-
cumulative stunting effect is shown dia-
grammatically in figure 62.
Aeration
The roots of a plant obtain the raw
materials, water and mineral nutrients,
which are carried upward through the
stem to the leaves. The tops act as fac-
tories, synthesizing the compounds re-
quired for growth and reproduction
from these materials and carbon dioxide
from the air. For roots to function
normally they must be supplied with a
source of energy and an environment
favorable for utilizing it. The top of the
plant provides the sugars and other
carbohydrates, which are transported
through the stem down to the roots,
where, through respiration, they supply
the energy necessary for root function.
Respiration, as in the case of animals,
requires oxygen and produces carbon
dioxide and water. Oxygen is also re-
quired for respiration in other parts of
the plant, but the supply there is nearly
always adequate. Because of the tiny
pore spaces in soil through which the
gases move, aeration (oxygen supply and
carbon dioxide removal) of the roots
can readily become limiting. A good soil
mix must insure the best possible aera-
tion consistent with other requirements.
The additional moisture retained by soil
in a container reduces the air space. It is.
therefore, important that container soils
[87]
Plant
Growth
Available
Soil
Moisture
Unavailable
Soil
Moisture
CONSTANTLY AVAILABLE
WATER SUPPLY
INTERMITTENTLY AVAILABLE
WATER SUPPLY
Time
Time
Fig. 62. Diagram of plant growth in relation to moisture availability. The plant constantly sup-
plied with water grows continuously. The plant exposed to occasional water deficit grows inter-
mittently, and is smaller.
Fig. 63. Diagram of plant growth in relation to mineral nutrient supply. The plant uniformly
supplied with fertilizer grows continuously and is larger than the one intermittently supplied.
An excessive application of fertilizer (at right) killed the plant.
Plant
Growth
Tissue
damage
Slight
excess
Favorable
supply
Deficiency
CONSTANTLY FAVORABLE
MINERAL NUTRIENT SUPPLY
VARYING
MINERAL NUTRIENT SUPPLY
Death
f
Fertilizer Application
Fertilizer Application
s \
p^v
\N.
Time
Time
[ 88 |
have a maximum porosity. It is pri-
marily by diffusion that gases move into
and out of a soil, though applications of
water may also be effective in displacing
soil air, particularly in containers (Sec.
9) . If the soil pore spaces are very small,
water will fill them and reduce aeration
until the water content has been lowered
by evaporation or transpiration.
Of additional importance is the fact
that a soil through which air does not
diffuse readily will also be difficult to
treat efficiently by fumigation or steam
(sees. 8, 9, and 11) .
Mineral nutrients
At the present time most green plants
are known to require at least twelve
chemical elements (nitrogen, phospho-
rus, potassium, calcium, magnesium,
sulfur, iron, zinc, manganese, copper,
boron, and molybdenum) that are ob-
tained from the growing medium by the
roots. Foliar feeding may be used to sup-
plement root absorption. A fertile soil is
one in which all of these elements are
present in adequate but not excessive
quantity. A good soil mix must therefore
contain them, or the growing procedure
must provide for their supply during
plant growth.
This function is made possible in part
through the breakdown of organic mat-
ter, native mineral soils, and fertilizers
in the complex activities of soil microor-
ganisms, as well as fixing atmospheric-
nitrogen to make it available to the plant
(Sec. 14). To this extent they are prop-
erly considered as a necessary part of
the soil environment of the plant.
As with moisture, it is important that
the supply of these minerals be continu-
ous rather than intermittent (fig. 63).
The greatest problem occurs in main-
taining proper nitrogen supply (Sec. 7).
DISADVANTAGES OF MULTIPLE SOIL MIXES
It is still the practice in some Califor-
nia nurseries to have a separate bin or
compost pile of a special soil mix for
nearly every crop grown. This is a costly
procedure beset with several serious dis-
advantages.
Labor requirement
Preparation of many small lots of soil
costs vastly more than does preparation
of a single large batch, and makes un-
economic the mechanization of handling.
If compost piles or bins are maintained
for each, the labor requirement becomes
very large.
Space utilized
Land area is required for the piles of
raw materials or compost, mixing areas,
and storage bins. It is not uncommon for
large nurseries in southern California to
use 1 to 2 acres for these purposes. Be-
cause of the real-estate pressures pre-
viously mentioned (Sec. 2), and the in-
creasing tax rates, land area must now
be used with greatest efficiency.
Variability of composts
Composts containing leaf mold, animal
manure, or turf will be highly variable
in composition because these materials
are themselves far from uniform. Fur-
thermore, if these ingredients are com-
posted, the degree of decomposition will
not be uniform in all lots at different
seasons, and the mixture thus would be
even more variable than before. With
these inherently variable mixtures, the
plant response often becomes so un-
predictable as to prevent scheduled pro-
duction.
Shrinkage in composting
Manure, used to supply organic matter
and nutrients, is not a good source of
either for nurseries. In California it is
[89]
likely to be more dehydrated than de-
composed, and the buyer accordingly as-
sumes the shrinkage. "Leaf mold" in
California usually means partly decayed
leaves, subject to a considerable loss in
composting. Because peat is largely de-
composed before it is dug, composting is
unnecessary and shrinkage during use is
comparatively minor.
Odor and flies during
composting
In residential areas unpleasant odors
and flies are likely to bring zoning re-
strictions. Compost piles are already
being discontinued for this reason in
some areas.
Scarcity of composting
materials
Because of the scarcity of deciduous
forests in California, the semiarid cli-
mate, and destruction from fires, leaf-
mold deposits are rare and generally
protected by law. Animal manure may
become scarce, and the nurseryman must
compete with mushroom growers and the
package-manure trade to get it. For these
reasons many nurserymen have prac-
tically ceased using these two materials.
In England and the humid parts of this
country, sod from turf or meadowland is
used in compost piles. In California, turf
can rarely be used because there are few
natural meadows, and land and water
are too valuable to be used only for a
turf crop.
Salinity problem
This serious problem, discussed in
Section 4, is important in the selection of
composting materials. During the decom-
position of leaf mold in place, in the
compost pile, or in the container, the
mineral content is made soluble, which
increases salinity. Consequently, Califor-
nia "leaf mold" is commonly high in
soluble salts, whereas in areas of high
rainfall these have been removed by
leaching. In one instance, leaf mold that
had been used for growing cattleya or-
chids in benches, was sold to nurserymen
for use in bedding plants. This decom-
posed material had excellent physical
properties, but because it had been
watered lightly without leaching, the
salts from the water and from fertilizers
had accumulated to an extremely high
level. When it was used in nursery soils,
seedlings were quickly and severely in-
jured by the soluble salts. Manures, by
their very nature, are always saline.
Post-treatment toxicity
This important disadvantage of con-
ventional soil mixes is discussed below.
Comparison with
U. C.-type mixes
By comparison with multiple soil
mixes, the use of a single one of the U. C.
type (Sec. 5) presents definite advan-
tages: it requires less labor and can be
more economically mechanized in the
handling operation; less storage space is
needed since compost piles are elimi-
nated; greater uniformity of mixture
and predictability of plant growth will
result; loss by shrinkage and leaching
during composting is reduced; scarce
materials, such as manure and leaf mold,
may be eliminated by using readily
available peat instead; some of the
sources of soluble salts may be avoided.
ATTEMPTS TO IMPROVE NURSERY SOIL MIXES
Progress in the art of compounding artificial conditions imposed by man.
nursery soil mixtures is but an expres- Empirical additions of different mate-
sion of the developing fundamental rials, or the formulation of various
philosophies of plant culture under the mixes, are of less permanent importance
[ 90 1
to nurserymen than is the evolution of
the ideas behind them. Viewed from this
angle there has been slow but steady
progress in the subject.
Man's earliest cultivation of plants
was undoubtedly in some sort of field
plots, and he found at a fairly early
period that growth was enhanced by ap-
plication of some type of fertilizer. Per-
haps he discovered that plants would
grow in containers when he was faced
with the necessity of moving some of
them to a new area during migrations. It
was then but a step to find that they
could be grown in that way very suc-
cessfully if fertilized and properly han-
dled. It is known that trees were grown
in large "boxes" or "pots" cut in rock
and filled with special soil in Egypt about
4,000 years ago. Frankincense trees were
brought from Punt (Somali Coast) to
Egypt in containers to be grown in gar-
dens about 3,500 years ago; that this was
carefully recorded as an outstanding
achievement suggests that it was one of
the earliest instances of plant nursery
operations (fig. 64 J.1 When man began
growing plants for ornamental use it was
natural that some should be grown in
containers to be taken into his home or
gardens.
When a practice is slowly developed,
there usually is little critical examina-
tion of the methods employed. Growers
of plants in containers adopted a very
complex series of soil mixtures for dif-
ferent crops. Although many growers
thought they had independently de-
veloped the ideal soil for a given crop,
there was no consistency between them,
as there should have been if the con-
clusions were valid. Sometimes this mix
was based on the soil that had been used
for an especially successful crop, the
1 The Temples of Neb-hepet Re' Mentu-hotpe
(2061-2010 B.C.) (Winlock, 1942), and Hat-
shepsGt (1520-1479 B.C.), Deir el-Bahri, near
Thebes (Naville, 1913). The Metropolitan Mu-
seum of Art, New York, directed the writers to
these examples.
possibility that some other factor may
have been largely responsible for the
superior results being ignored. In other
cases this was based on the fallacious as-
sumption, already discussed, that the
only proper soil for a plant is one similar
to that of its native habitat.
The J. I. Composts
Tests at the John Innes Horticultural
Institution in England demonstrated that
a single soil mixture could, with minor
modifications, be used for growing a
wide range of plants. The usual battery
of special mixes was, therefore, unneces-
sary. The importance of this finding has
slowly been appreciated by growers in
England, Europe, and this country. This
development constitutes one of the im-
portant conceptual landmarks in the sub-
ject of nursery soils. For the English
grower this has been crystallized in the
J. I. composts, as follows:
Seed compost
7 parts composted medium loam, by volume
3^j parts peat, by volume
3^/2 parts coarse sand, by volume
To each cubic yard of the above is added,
with thorough mixing
2 pounds of superphosphate (18 per cent
phosphoric acid)
1 pound of chalk (calcium carbonate)
Potting compost
7 parts composted medium Loam, by volume
3 parts peat, by volume
2 parts coarse sand, by volume
To each cubic yard of the above is added,
with thorough mixing
2 pounds of hoof and horn meal (13 per cent
nitrogen)
2 pounds of superphosphate (18 per cent
phosphoric acid)
1 pound of sulfate of potash (48 per cent
potash)
1 pound of chalk (calcium carbonate)
The medium loam consists of the com-
posted residue of a 4- to 5-inch layer of
turf removed from pastures or meadows;
it contains 2 to 7 per cent humus and
only enough clay "to be slightly greasy
when smeared". Sandy, heavy, or cal-
careous soils are said to be unsatisfac-
tory.
[91]
i>A>jf»,
r
mm
-ifif]
w,\\v\\
yyiStl I
/ ///V^7/ / / /AC//// / / / /
'2Jjlj.ll )j)iU, J/ / / / / /jhA^ufij / / / / / / / / / / //_.v '/'// //////////'/) //)//////////// a?) i
In order to avoid toxic residue from
this mix it was found necessary to steam
the composted loam before adding the
peat, then to mix them and add the lime
and fertilizers.
The following disadvantages are in-
herent in the J. I. composts: (1) some
variability necessarily results from the
use of composted nonuniform turf soil;
(2) the necessary composting of the turf
loam before using in the mix takes both
time and space; (3) there is a high labor
requirement in handling the composting
operation; (4) meadowland turf is not
commonly available in most areas in this
country; (5) they contain coarse sand,
which unnecessarily increases the
weight; (6) a toxic residue is apparently
produced if the soil is steamed after mix-
ing. If toxicity is prevented by aging
after steaming, the recontamination
problem is increased and a storage prob-
lem is created; if it is prevented by
steaming the components separately and
then mixing, the recontamination prob-
lem is still increased.
Evolving the U. C.-Type Mixes
Work was begun in the Department of
Plant Pathology, University of Califor-
nia, Los Angeles, in 1941 to find a better
soil for growing plants in containers
than that then available. Because of the
scarcity of turf for composting, the toxic
residue after steaming, and the salinity
problem, it was not possible to use the
J. I. compost system. A substitute was
therefore sought. At first a fine sandy
loam was selected, and to this was added
leaf mold and horse manure in the ratio
of 10:2:2. Because of the variability of
these organic materials, and the potential
danger of excess salts in them, Canadian
peat was soon substituted for them in the
ratio of 3 parts of peat to 7 parts of
sandy loam. Mineral fertilizers were
added before steaming. No toxic effect
was observed in any of a wide range of
plants grown in this mix, even when
planted immediately after steaming.
Work to this stage of development was
reported in 1948 (Baker, 1948). This
mix was used for several years.
Further developments of the mix were
undertaken by the Department of Plant
Pathology in 1949 when Philip A.
Chandler, who had been at the John
Innes Horticultural Institution in 1935-
1937, joined the group. 0. A. Matkin co-
operated in the work after 1950, particu-
larly on physical and chemical aspects of
the soils. Five representative formula-
tions of two ingredients, fine sand and
peat, with a number of variations of
fertilizer additions are now suggested
(Sec. 5). Collectively these have been
named the U. C. soil mix, and sometimes
erroneously called "the UCLA blend,"
"Cal-Mix," "light soil mix," and "Calsoil
Mix."
The concepts behind this system, how-
ever, are of greater permanent value to
the industry than the formulas. Toxicity
after steaming has been eliminated,
probably through the use of fine sand
without appreciable clay or organic-
matter fraction, and of peat free of
readily decomposable organic matter,
and through maintenance of low con-
centrations of soluble salts by using low-
conductance ingredients and fertilizers
not readily decomposed by steaming.
The mixes are reproducible because they
use only ingredients that are readily
available in uniform quality. Compost-
ing is eliminated because the organic
Fig. 64. Culture of plants in containers was perhaps first practiced by the Egyptians 3,500-
4,000 years ago. Top, frankincense trees growing in pots. Middle and bottom, frankincense trees
in containers being introduced to Egypt from the Somali Coast. This is one of the early recorded
instances of plant introduction. Recorded in the Temple of Hatshepsut, Deir el-Bahri, near Thebes.
(From Naville, 1913.)
[93]
matter used is already largely broken
down, and the fertilizer is uniformly dis-
tributed through the mass by mechanical
means rather than "weathering". Plant
growth in the mixes is uniform in size
and time. Many kinds of plants obtain
the necessary nutrients in uniform sup-
ply from these mixes for several weeks
before additional fertilizer is needed.
When organic nitrogen is used, plants
are supplied a minimum level of nitro-
gen below which the supply does not fall.
The organic nitrogen is in a form only
slightly decomposed by steaming. It is
quite possible to procure and mix the
uncomposted ingredients, steam them,
and use the soil for planting, all in the
same day. This fact, plus the uniform
results, makes possible for the first time
truly scheduled production and mechani-
zation.
In England, the pasteurized J. I. com-
posts have been placed on the market
by commercial suppliers in quantities
varying from a bag upward. This may be
the ultimate development with the U. C-
type mixes, with the grower no more
"involved in the soil business" than he
is presently in the seed business. Expe-
rience in California has shown, however,
that there are several problems yet to be
solved before this goal can be success-
fully achieved here.
The Einheitserde
Still a different solution of the prob-
lem of soil treatment toxicity has been
developed in Germany. The Einheitserde
(Standardized Soil) developed by Dr. A.
Fruhstorfer of Hamburg and introduced
in 1948, is now marketed by several
companies in that country. The mix is
half peat and half well-aggregated sub-
soil clay, to which are added ammonium
sulfate, superphosphate, and potassium
sulfate. Half as much fertilizer is added
to seed soil (P-Erde) as to potting soil
(T-Erde). Lime may be added to main-
tain pH 5 to 6. These materials are mixed
together and used without treatment, be-
cause the peat and the subsoil are largely
free of weeds, organisms, and decom-
posable organic matter. This single mix
is used for a wide range of plants.
This seems to be a drastic method of
avoiding the treatment-toxicity problem,
and still involves the disadvantages of
clay soils described in this section, and
of ammonium accumulation (Sec. 7).
The assumption is unwarranted that peat
is free of organisms capable of causing
disease. Recent German studies have
shown that the mix may be infested with
pathogens during storage (Danhardt and
Ramsch, 1955) and handling. Neither is
the organism carryover on containers
prevented. Granting that this method is
better than using ordinary untreated
composts, it still leaves much to be de-
sired.
In England, a patent application for a
compost similar to the Einheitserde has
recently been published (Allerton and
Ray, 1954). The mix consists of 1 to 2
parts by volume of sphagnum peat moss,
1 to 2 parts of fine vermiculite, 1 to 2
parts of heavy clay, plus fertilizers. An
example of the fertilizers is to use 8
ounces per bushel of a mixture of 2 parts
by weight of magnesium sulfate, 2 parts
potassium nitrate, 3 parts ammonium
sulfate, and 4 parts single superphos-
phate. This compost apparently is not
yet being sold.
SOIL TOXICITY IN RELATION TO TREATMENTS
A drawback sometimes encountered
from chemical or steam treatment of soil
il the resulting injury to plants grown in
it. The type and severity of the injury
varies with the soil, the treatment, the
plant, the time and handling of the soil
after treatment, the environmental con-
ditions, and perhaps other factors. Symp-
toms may be stunting of the plant, dis-
coloration, necrosis, and abscission of
leaves, death of the plant, or reduced
seed germination. The toxic effect may
be temporary or last several months,
particularly if the soil is kept sterile or
dry. When a proper soil mixture is used
this toxicity does not appear, and there
is no reason to have this problem.
Substances Involved
The many investigations that have
been concerned with the nature of the
toxin warrant the conclusion that several
injurious agents may be involved. Briefly
these are as follows.
Accumulation of ammonium
Bacteria that decompose ammonium
are non-spore-forming and more sensi-
tive to heat and many chemicals than the
ammonifying organisms which convert
organic nitrogen to ammonium. Treat-
ments may thus cause the accumulation
of ammonium, since there is a delay in
conversion to nitrate. As discussed in
Section 7, accumulation of ammonium
may reach toxic levels in 2 weeks and
last for 6 to 8 weeks or more.
If leaching of the soil reduces toxicity,
ammonium may not be the factor in-
volved because: if leaching is successful
soon after steaming, the ammonium
usually has not yet reached toxic levels;
if leaching reduces toxicity in soil
treated some weeks before, the am-
monium may largely remain in the soil
instead of being removed. Ammonium
may, however, bs involved if prompt
planting after treatment prevents injury,
since the transplants might be carrying
nitrifying bacteria that would convert
the ammonium, and the plants might
keep the ammonium at a low level by
absorbing it as formed, both of which
would prevent accumulation.
Water-soluble organic matter
Organic matter is rendered water-
soluble (broken down) in varying de-
grees by heat and chemicals, but the
nature of the process or the products are
little understood. These materials are
removed by leaching immediately after
steaming and may be involved where
benefit is derived from such treatment.
Our experience has confirmed reports
that soil mixtures high in readily decom-
posable organic matter (manure, leaf
mold, compost, some black peats) gen-
erally give greatest toxicity from steam-
ing. Highly organic soils also give
greatest residual toxicity to bromine-
sensitive plants (for example, carna-
tions) from methyl bromide fumigation.
Available manganese
Soils, particularly of the acid lateritic
type, may release toxic amounts of man-
ganese when steamed. In Hawaii this
causes severe injury to some crops (let-
tuce, cowpeas) in steamed soils. Leach-
ing of treated soils removes this in-
jurious factor.
Increase of total soluble salts
Some soil ingredients may release
enough adsorbed salts when steamed to
produce plant injury. Thus, our tests in
1944 showed an increase in conductance
(EC x 105 at 25° C on a 2:1 extract)
from 117 and 151 to 228 and 213, re-
spectively, in two series using a highly
organic mix plus cow manure, after 45
minutes' steaming at 212° F. Leaching
removes these toxic salts and is com-
monly practiced for this purpose.
Other agents
Other agents that have been reported
as resulting from soil steaming are: in-
crease in water-soluble salts of calcium,
copper, magnesium, potassium, zinc,
phosphorus, and aluminum; altered pH;
decreased iron and nitrate; osmotic con-
centration of soil solution: modified ab-
sorptive capacity of soil for water, gases,
and salts.
[95]
Avoiding Post-Treatment
Toxicity
Several methods of dealing with this
toxicity problem have been discovered
and utilized under commercial condi-
tions.
Choice of soil mixture
The best method is to avoid the trouble
by using a soil mixture which does not
form toxins after steaming or chemical
treatment (sees. 5 and 7). All the types
of toxicities resulting from heating soil,
with the possible exception of ammonium
accumulation, are eliminated by using a
U. C.-type soil mix. The ammonium
problem may easily be kept under con-
trol by methods explained in sections 5
and 7. The J. I. composts and the Einheit-
serde mentioned earlier evade treatment
toxicity at the expense of increased risk
from disease loss; the U. C. system both
eliminates the problem and enhances
protection from disease. Since there are
also other advantages in a soil mix of
the U. C. type, there is little valid reason
for using a soil that requires corrective
measures for post-treatment toxicity. In-
terest in this toxicity problem is now
largely academic, since the choice of
proper ingredients makes it of no prac-
tical concern.
Leaching of the soil
Leaching is the present most common
method of reducing soil toxicity, and is
often quite effective. However, it puddles
the soil, creates a flood in the green-
house, removes soil nutrients and makes
fertilization necessary, increases the re-
contamination hazard, delays planting
operations, and increases cost of labor,
water, and fertilizers. It is an expensive
and messy solution of an unnecessary
problem. It is not very effective against
accumulated ammonium. Gypsum (cal-
cium sulfate) may be added to facilitate
the leaching of ammonium from the soil
(Sec. 7).
Aging of the soil
Steamed soil is sometimes left for
several weeks after treatment to reduce
toxicity, presumably through reestab-
lishing a biological balance in the soil.
In some cases it is steamed in the fall,
left all winter, and used in the spring.
Among the obvious disadvantages of this
method, however effective, are the ex-
treme recontamination hazard, the delay
in operations, cost of storing idle soil,
and the expense of additional handling.
Planting immediately
after steaming
This recent method may have merit
when ammonium accumulation is the
toxic factor involved. There are, how-
ever, some plants that are sensitive to
ammonium (Sec. 7), and these should
not be used in this way. See also "Ac-
cumulation of ammonium," above.
CRITERIA FOR PHYSICAL INGREDIENTS OF SOIL MIXES
Because of the foregoing facts, it is
necessary to select ingredients which will
perform the required functions and
satisfy certain other practical and eco-
nomic requirements of the growing op-
eration. Characteristics of each potential
component of the soil mix are discussed
below and summarized in figure 65. The
first four characteristics concern factors
which cannot be improved by mixing
with one or more other ingredients. If a
component fails to satisfy any one of
these conditions it is a hazard to the use-
fulness of the mix. The last nine char-
acteristics are, however, subject to altera-
tion or improvement by proper mixing of
ingredients. Mixtures of fine sand and
peat moss approach the ideal.
[ % i
Characteristics
E
o
o
—J
a
u
</5
-a
c
D
VI
<u
T3
C
o
m
4>
0
o
U
4)
>
O
6
4>
4>
a.
"5
u
'e
>
13
O
E
4)
4)
C
O
o
E
0
4)
a.
o
Q.
E
o
u
3
T3
O
lO
o
-Q
"a
B
3
o
6
3
0)
u
Si
>
o
00
o
o
c
o<5
c
0
l/l
d)
c
LL.
X
'e
0
2
Readily available
in uniform grade?
!K2g
1
Chemically
uniform?
Stable to steam
and fumigation?
9
9
•
9
•
9
9
9
Easily made into
uniform mix?
■
j
Good aeration
assured?
?
■
9
9
9
9
Resistant to loss of
nutrients by leaching?
9
Fertility
low?
9
9
9
•
1
Relatively
inexpensive?
Moisture retention
reasonably good?
9
Light in weight?
(Low Density)
9
Shrinkage in storage
negligible?
9
1
1
■
9
Gypsum or lime
required?
?
9
•
9
•
9
'
Micronutrients
adequate?
•*
9
9
9
9
9
9
9
9
9
9
9
9
9
9
9
9
yes
unknown or unpredictable
intermediate
~o a
a. -c _q -Q
I
4) O . — .
-5 'x o
t -a -£
<u -a a
a. D _c
S fc-f
a
4)
I
Fig. 65. Criteria for selecting the physical components of the U. C.-type soil mixes. Fine sand
is the best of the inorganic ingredients. Peat moss, sawdust, ground bark, rice hulls, and shav-
ings are best among the organic constituents.
Is it readily available
in a uniform grade?
There are few inorganic planting ma-
terials which are readily available in a
uniform grade. Clays, silts, and loams
are apt to be quite variable in particle
size, degree of aggregation, and mineral
content. A unique, reasonably uniform
source material, however, is naturally
available in the fine sand which has been
deposited in certain areas by wind,
water, or both. Many of the rolling
coastal and interior California hills con-
tain almost pure deposits of fine sand.
They are also frequently found as sub-
soils, drift sands, desert sands, and lake
sands. In quarry operations supplying
coarse sand and gravel to the construc-
tion trades, man has often artificially
separated the other components of a soil
from the fine sand and left relatively
pure deposits of it. The separation is gen-
erally made by screening and water
washing, which remove the silt, clay, and
fine sand from the coarser materials. The
silt and clay float off, leaving deposits of
pure fine sand. These deposits are fre-
quently called "silt," a misnomer. Since
considerable variation may occur from
area to area, the materials should be
carefully inspected before making a final
selection.
Among the organic physical compo-
nents are various types of peat moss, ma-
[97]
nure. leaf mold, composts, and others
such as the plant by-products (rice hulls,
sawdust, shavings, ground bark). Sphag-
num peat mosses of the European or Ca-
nadian type are commonly available in
adequate quantities, and in uniform and
reliable quality. The same cannot be said
of leaf mold, manures, composts, and
some other types of peat. Leaf mold was
largely used in the past, particularly by
growers in Europe and eastern United
States, because they had access to con-
stant and readily available supplies, and
the material was generally well decom-
posed and leached. In many areas of
California it is illegal to remove leaf
mold from its natural source. The plant
by-products mentioned above may not be
so generally available but may be fairly
uniform in grade where they are ob-
tainable.
Is it chemically uniform?
To be reliable as a basic component
of the soil mix, each ingredient must be
reasonably uniform in soluble and po-
tentially soluble constituents. Each in-
gredient of a soil mix should be non-
toxic to plants if used alone. Again fine
sand and peat moss offer a ready answer,
for they are both almost certain to be low
in soluble constituents and relatively in-
capable of release of such materials.
Other inorganics may or may not have
these properties. Organics of the leaf
mold, manure, and compost type are
completely unreliable in this respect.
These and many of the sedge peats, such
as the black peats from semiarid regions,
have frequently been found to be saline.
Many of the plant by-products are uni-
formly low in soluble and potentially
soluble minerals. On the other hand, they
may actually tie up such elements as
nitrogen during their decomposition in
soil.
Is it stable to steam or
fumigation treatment?
Stability to treatment is one of the
most important considerations, and was
one of the primary reasons for the de-
velopment of a reliable soil-mix system.
Unless the mix is stable to soil treatment,
all the benefits obtained by destruction
of pathogens may be lost by plant dam-
age from toxic materials produced in the
soil. The most common toxic materials
released by such treatment are excessive
ammonium, water-soluble organic mat-
ter, manganese, or soluble salts, as point-
ed out earlier in this section. This type of
problem does not occur where the soil
mix contains fine sand, peat moss, saw-
dust, shavings, bark, or rice hulls, but
may occur in soil mixes containing
loams, leaf mold, manure, and composts.
Is it easily made into
a uniform mix?
Ease of mechanical mixing and uni-
formity of plant growth are important
considerations in the selection of soil in-
gredients. Many growers in central Cali-
fornia have purchased expensive grind-
ing equipment to break up the clods in
clay soils, an operation eliminated by
using fine sand. In fact, the presence of
hard lumps in the soil is evidence that it
is unsuitable for use in the mix.
Organic materials such as peat moss
may sometimes be passed through a
shredder to break up the compressed
bales, but this is not an expensive or even
a necessary operation, for it can be
broken up fairly readily by hand. Some
brands of Canadian peat moss are now
packed with a thin sheet of polyethylene
as an inner lining to the package. This
reduces water loss and keeps the peat in
a slightly moist condition, making it
easier to break up and mix. Some grow-
ers have been using redwood fiber, a
bark product, which is difficult to make
into a uniform mix regardless of how it
is handled. Most of the other ingredients
of a U. C.-type mix are easily blended
with one another.
Is good aeration assured?
Because of small pore size, clays and
sills lend to have poor aeration under
[98 1
some conditions. The use of organic mat-
ter, particularly peat moss, can greatly
improve this shortcoming. Fine sand,
and the coarser grades of sand and
gravel are individually well aerated. It
should be pointed out, however, that a
mixture of fine and coarse sands with
relatively small amounts of silt and clay
can become very compact, and thus
poorly aerated. This is best illustrated by
the analogy of making concrete: par-
ticles of various sizes, ranging from sand
to gravel and rock, are mixed with water
and a little cement (powdery, claylike)
to form an impervious product upon set-
ting. A product of uniform particle size
offers little opportunity for cementing ac-
tion; for illustration, one might consider
the difficulty of trying to make concrete
of buckshot.
Most organic materials are favorable
to good aeration. If, however, these are
sufficiently decomposed, a "mucky" con-
dition may develop which is similar to
clay in its ability to obstruct air move-
ment. Leaf molds and manures reach this
stage quite rapidly, as compared with
peat moss or shavings. Many azalea
growers are finding it advantageous to
include shavings in their beds of peat
moss in order to insure good aeration as
the peat decomposes, and as weather be-
comes cold and wet.
The tiny pores in a clay or silt soil can
become completely filled with water,
leaving no space for air. On the other
hand, the considerably larger pores in a
sand or a sand and peat moss mixture
cannot be fully occupied by water unless
drainage is prevented. Both water and
air can occupy the pore spaces of a
medium consisting of a uniform grade of
sand. A well-aerated soil is a well-drained
soil.
Is it resistant to
leaching of nutrients?
Loams, clays, humus, and most unde-
composed organic materials are retentive
of certain elements of importance in
mineral nutrition. This property is one
of base exchange and is peculiar to the
above-mentioned components. Ions such
as ammonium, potassium, calcium, and
magnesium may be held by the particles
in available but nonleachable status.
Another factor to consider in leach-
ability is the amount of water it takes
to actually displace the soil solution. In
comparing a silt and a gravel, it is ob-
viously easier to flush all soluble ma-
terials out of the gravel than out of the
silt, though neither has an appreciable
base-exchange capacity. Thus, a fine
sand is slightly retentive of nutrients and
the coarser materials much less reten-
tive. Organic matter is all more or less
retentive. A mix of fine sand and peat
moss can be prepared to satisfy this re-
quirement quite efficiently. Such a mix
would have a base-exchange ability and
moisture capacity comparable to a sandy
loam without the hazards introduced by
the clay content.
Is the fertility low?
It may seem unusual that there should
be an advantage in using materials of
known low fertility. The explanation is
that if fertility is low, it is simple and in-
expensive to add enough of the correct
fertilizers to bring it up to the desired
level; whereas if fertility is high or un-
known, obviously the problem of what
and how much to add can be resolved
only by a complete soil analysis or by
growing trials. In the case of loam,
clay, silt, leaf mold, manure, or com-
posts there is almost certain to be an un-
known level of fertility, or even possible
salinity. The sands and peat mosses are
relatively low in fertility. Wood shavings
and sawdust are very low in fertility,
and organisms which cause their decom-
position utilize some or all of that nor-
mally supplied. Ground bark has fre-
quently been found to be well supplied
with phosphorus and potassium in an
available form. Rice hulls have been
found to contain considerable potassium
[99]
in soluble form. Since a mixture of fine
sand and peat moss provides a known
low starting point, reliability of the final
mix is assured.
Is it relatively inexpensive?
Depending upon the value of the crop
to be grown, the answer here may be
quite variable. In general, the inorganic
products such as clay, loam, fine sand, or
gravel are inexpensive, hauling often
being the main cost. Peat moss, manure,
leaf mold, and composts may be con-
siderably more expensive, but far
from prohibitive. Composting operations
greatly increase the cost of handling.
Composting area further increases ex-
pense by enlarging the space required for
the growing operation. As mentioned
earlier, when fine sand and peat moss are
used it is possible to make up the mix,
treat, and plant on the day of delivery.
The plant by-products such as sawdust
and shavings are fairly inexpensive,
sometimes even free. Mixtures of fine
sand and peat moss are generally less ex-
pensive than other soil preparations in
cost of labor.
Is moisture retention
reasonably good?
As discussed earlier in this section,
moisture supply is of major importance,
and the ability of a material to retain
moisture for a reasonable length of time
becomes important. Otherwise too much
labor is required for maintaining an ade-
quate supply for plant growth. Clays,
silts, peats, and other organic materials
are generally high in their capacity to
retain moisture, peat being highest of
all in this property. Peat moss is a logical
material to include in a sandy type mix
because it increases water and mineral-
nutrient retention, and further improves
aeration.
Is it light in weight?
Current practices of marketing and
shipping plants in containers make it
quite important that the weight be kept
as low as possible. Light-weight growing
media are confined largely to the organic
materials, with peat moss, shavings, and
sawdust among the lightest. Sands and
gravels constitute the heaviest materials.
Perlite and vermiculite are light-weight
inorganics, but are rather expensive. A
low-density growing medium is of con-
siderable importance in any operation in
which containers are lifted or moved
during the growing period. A U. C.-type
soil mix will have about the same density
as the usual compost mix, and may, if
large proportions of peat are used, be
considerably lighter.
Is shrinkage in
storage negligible?
Many materials have to be held in
storage until the grower is ready to use
them.
It has been reported that 25 to 66 per
cent of the organic matter (and total
volume), 50 to 70 per cent of the nitro-
gen and potassium, and 33 to 50 per cent
of the phosphorus are lost in animal ma-
nures during outdoor storage. A ton of
fresh manure containing 500 pounds of
organic matter, 25 pounds of nitrogen,
25 pounds of potash, and 8 pounds of
phosphate may produce 1,100 pounds or
less of material suitable for nursery use,
containing only 250 pounds of organic
matter, 10 pounds of nitrogen, 10
pounds of potash, and 5 pounds of phos-
phate.
Leaf mold in California usually means
partly decayed leaves, subject to a con-
siderable but undetermined loss in com-
posting. In New York it was found that
oak leaves shrank 33 per cent, maple
leaves 35 to 40 per cent, and wheat straw
25 per cent during composting. Because
peat is largely decomposed before it is
dug, composting is unnecessary and
shrinkage during use or storage is com-
paratively minor.
If nothing else, shrinkage is an eco-
nomic consideration, for it increases the
[100]
cost of the component which is so re-
duced. If decomposition is not completed
before using the material, the process
will continue in the container, causing
an erratic nutrient supply for the crop.
For this reason organic materials are
generally decomposed before use.
Is gypsum or lime required?
Although gypsum and lime contain
certain plant nutrients, they are usually
used as soil amendments. Highly acid
materials such as peat moss and wood
by-products can be neutralized by the
addition of the proper amount of lime. If
dolomite lime is used, both calcium and
magnesium are supplied in addition to
the neutralizing action obtained. If the
component is not too acid, it may be de-
sirable to use gypsum to supply calcium
and perhaps reduce the potential danger
from alkaline (high-sodium or artificially
softened) water. Mixtures of fine sand
and peat moss usually require the addi-
tion of lime.
Are micronutrients adequate?
This is one of the most difficult ques-
tions to answer. These elements are re-
quired in such minute amounts that they
may normally be supplied in adequate
quantity by the basic physical compo-
nents. Organic ingredients had to be
supplied with the elements in order to
have developed in the first place. In ad-
dition, water used for irrigation may
supply some elements, and fertilizers also
frequently carry micronutrients as im-
purities. Except for long-term growing,
micronutrients will not usually constitute
a problem. If ever found to be important,
they can be added (see "Micronu-
trients," below).
SELECTING INGREDIENTS FOR U. C. MIXES
The final mix may consist of any one
or combination of suitable ingredients.
// the mix is a good one, nearly all plants
may be grown in it. If it is a poor mix,
only those which are tolerant of the poor
features may be grown in it.
The foregoing considerations have
narrowed the choice of the physical com-
ponents down to a very few which will
satisfy the requirements. The selection
of fine sand as an inorganic fraction
seems obvious. The selection of the or-
ganic fraction is confined to sphagnum
peat moss or possibly some of the other
materials mentioned. It should be
pointed out that some of the artificially
produced inorganic materials such as
perlite and vermiculite also offer the de-
sirable properties of fine sand. Their
cost is, of course, much higher, but they
may have particular uses under certain
circumstances. For practical purposes,
therefore, the standard system is based
on the use of fine sand or peat moss of
the sphagnum type, or both.
Fine Sand — Specifications
"Fine sand" applies to soil particles of
a certain size. As used here, the maxi-
mum and minimum dimensions are 0.5
mm (approximately 1/50 in.) and 0.05
mm (approximately 1/500 in.), respec-
tively. According to U. S. Department of
Agriculture standards, this range of par-
ticle sizes includes the classifications:
medium sand, fine sand, and very fine
sand. It has not seemed essential from a
practical standpoint to thus restrict the
specification of particle size limits. As
used here, therefore, the term fine sand
will be understood to also include the
classifications, medium and very fine
sand. The relative diameters of the par-
ticle sizes are shown diagrammatically
in figure 66.
[101]
©
©
Clay
(0 - .002 mm)
Silt'
(.002- .05 mm)
Very fine sand
(.05-0.1 mm)
Fine sand
(0.1 -0.25 mm)
Medium sand
(0.25 - 0.5 mm)
Desirable
particle
size range
for soil mix
Coarse sand
(0.5 -1.0 mm)
Fig. 66. A comparison of relative sizes of soil particles, according to the United States Depart-
ment of Agriculture system. The circles represent the maximum and minimum for each class.
I 102]
If materials are being obtained from
gravel quarries, the common designation
for fine sand is "minus 30 and plus 270."
These figures refer to screen sizes and
mean that the material passes a 30-mesh
screen and does not pass a 270-mesh
screen.
The identical grade or grades of fine
sand will not be available everywhere,
since the degree of purity (freedom from
coarser and finer materials) is certain
to vary. It is, therefore, necessary to set
up specifications or permissible percent-
ages of particle sizes other than those
included in this fine sand classification.
The least critical factor from the stand-
point of soil structure is the amount of
material present which is coarser than
the fine sand. If silt and clay are present
in minimal amount, the inclusion of
coarse sand and fine gravel will serve to
make the mix more porous, heavier, and
lower in moisture retention. Too coarse
a sand will permit the soil to fall away
from the roots during transplanting. If
silt and clay are present in quantity, the
presence of coarser materials will make
the mix more susceptible to compaction
and cementlike properties, as already ex-
plained.
The selection of the proper soil source
by the nurseryman is of the greatest prac-
tical importance. After he becomes ac-
customed to the appearance and feel of
the correct material, he may find it fairly
easy to distinguish good from poor
sources. To familiarize himself with the
proper type of soil, the nurseryman
should examine samples of suitable fine
sand either in use by other growers or
exhibited by the Agricultural Extension
Service. Having found a suitable source,
a grower should retain a sample for
future comparison.
The safest procedure is to actually
measure the percentages of the important
particle sizes. This type of test is made
by many commercial laboratories, but
the requirements here are not so exact-
ing that a grower cannot carry them out
if he desires. A high degree of accuracy
is not required for practical purposes.
The soil to be used in the tests should be
oven- or sun-dried. The equipment re-
quired is listed as "Soil Testing Equip-
ment" in the Appendix.
For purposes of the soil mix a de-
sirable material will have the following
limits:
Coarse sand — should not exceed 12 to
15 per cent, preferably less.
Fine sand — should not be less than 70
per cent, preferably 85 per cent or
higher.
Silt plus clay — should not exceed 15
per cent, preferably lower.
The results of physical analysis of a
number of sandy soils which have been
in use are given in table 10.
The basic soil should be low in organic
matter, because (1) toxins are not then
produced on steaming, (2) it supplies a
known base to start from in adding peat,
(3) the organic fraction might throw off
the determinations of particle size.
Determination of coarse
sand and gravel
1. Weigh 100 grams of soil into a quart jar,
add a pint of tap water, and shake vigor-
ously to disperse the fine materials.
2. Obtain the dry weight of the sieve (32
mesh, or 0.5 millimeter diameter holes)
and then wash the dispersed soil through
the sieve. Use a gentle flow of water from
a tap and gently swirl. Avoid flushing soil
over the edge of the sieve.
3. When no more material will come through
the sieve, dry it in an oven or in the sun
and reweigh sieve and contents.
4. The percentage of coarse sand and gravel
is equal to the gain in weight in grams of
the sieve with contents.
Determination of silt and clay
1. Fill the hydrometer jar about half full of
distilled water and add 10 milliliters of
saturated sodium oxalate solution. This
saturated solution is prepared as follows:
To a pint jar partly full of distilled water
add V-i pound of sodium oxalate. Shake
occasionally over a period of several days
before use. Use the clear liquid from the
[ 103 ]
Table 10. Physical Analysis of Sandy Soils Used by Nurserymen
Per cent of various particle sizes
Desirability
Soil sample No.
Coarse
particles
Fine
sand
Silt plus
clay
for
soil mix
1
2
3
4
4.1
3.7
7.3
4.6
42.1
10.0
3.7
92.4
76.1
82.7
91.7
32.9
71.8
90.7
3.5
20.2
10.0
3.7
25.0
18.2
5.6
Excellent
Poor
Good
Excellent
5
6
Very poor
Fair
7
Excellent
No. 1. Field soil with good drainage and no compaction. Coastal bluff in Santa Barbara area.
No. 2. Field soil from same area as no. 1, but with poor drainage and a tendency to form compacted zones
unless large amounts of organic matter are used.
No. 3. "Silt" from a quarry operation in the Monrovia area. The washing process results in the removal of
most of the coarse materials for sale as building sands and the clay is washed away. The so-called
"silt" or waste material is actually fine sand. Mixes made from this product are of good physical texture.
No. 4. Deposits of wind-blown origin. Large hills in Palos Verdes area. Also obtainable as waste "silt" from
local quarry operations in this area.
No. 5. A soil from the Redondo area which, when used in the soil mixes, gave unsatisfactory results because
of a tendency to set like concrete. Note the particle size distribution.
No. 6. A top soil from the Torrance area. Gave good results with high peat-moss content, but not quite so good
with mixes low in organic matter.
No. 7. A wind-blown sand from the Colma (San Francisco) area. Excellent structure in the soil mixes.
top of the jar. Distilled water may be
added to replace that used so long as
crystals are still present in the jar.
2. Weigh another 100 grams of the dry soil
and pour into the jar. Allow to stand for
5 or 10 minutes.
3. Disperse the soil in the water by placing
the palm of the hand over the mouth of the
jar and inverting. Repeat this several times
in a period of 20 minutes. If necessary, add
more sodium oxalate to keep the silt and
clay fraction dispersed after mixing. When
properly dispersed the liquid will remain
quite muddy after standing about 5
minutes.
4. Add distilled water to the hydrometer jar
until the total volume of liquid is up to the
1,000-miIliliter mark.
5. Invert the jar several times and quickly
place it upright on a level bench and note
the time on the second hand of a watch.
6. Place the hydrometer gently in the column
and allow it to come to equilibrium. At
exactly 40 seconds after setting the jar
upright take the reading of the liquid level
on the hydrometer stem. This reading,
when corrected for temperature, is the per-
centage of silt phis clay.
7. After taking the hydrometer reading and
removing the hydrometer, measure the
temperature of the liquid in the jar. For
< \ery degree above 67° F, add 0.2 to the
reading obtained on the hydrometer. For
every degree below this temperature, sub-
tract 0.2.
Determination of fine sand
The percentage of fine sand can be calculated
from the data obtained above. The fine-sand
fraction is equal to the sum of the two deter-
mined fractions (coarse sand and gravel, plus
silt and clay) subtracted from 100.
The hydrometer test outlined above is subject
to increasing error as the silt, clay, and organic
content of the soil being tested increase.
Ordinarily, the fine sands are low enough in all
of these to make such errors negligible.
Peat Moss
The only other basic component of the
standard mixes is peat moss of the sphag-
num type obtained from Canada, Europe,
and some parts of northern United
States. California hypnum peat moss has
also proved to be satisfactory. In general,
other types of peat are too uncertain in
chemical and physical composition to be
included in standard mixes. For instance,
many of the sedge peats of arid areas
(for example, the black peat of coastal
[104]
California ) are saline. Some are infested gins. Unless the soil is put to use within
with undesirable organisms. a week the nitrogen released may become
The peat moss should be finely ground excessive for plant growth. Materials
so that it will readily mix with the other which have been used as organic sources
component, fine sand. The mixing opera- of nitrogen in the U. C. system of prepa-
tion is greatly facilitated by moistening ration are:
the peat a day or two beforehand. Approximate per cent
Material of nitrogen
—■ B • ^»i_ • _i ■_ ^ j:^_*. Hoof and horn meal 13
The Basic Chemscal ingredients D1 , , ...
Blood meal lo
In order that plants may grow prop- Cottonseed meal 7
erly, mineral nutrients must be included Castor pomace . . 6
, . ,. rpii i • l • Urea-formaldehyde resin So
in the growing medium. Ihe basic physi-
cal ingredients that have been recom- Anyone contemplating the use of urea
mended are almost certain to be low in or urea-formaldehyde fertilizers should
the required elements, providing a note the warning about possible biuret
known starting point. The problem of injury on p. 79.
providing a medium containing a rea- There may be other acceptable ma-
sonable balance of required nutrients is terials, but so far they have not been suf-
easily met by the addition of a few com- ficiently tested to justify their inclusion.
mon fertilizers. The material most used so far has been
hoof and horn meal.
Nitrogen There is little point in adding the am-
The proper use of nitrogen is probably monium form of nitrogen to the mix. As
the most important factor in the nutri- explained in Section 7, this form is toxic
tional success or failure of this or any to some plants when present in sufficient
system of soil mixes. A more complete quantity. Further, it will be present in
description of the complexities is pro- some quantity where organic nitrogen is
vided in Section 7. Briefly, nitrogen can supplied, since it is the first major prod-
be supplied in any one of three forms, or uct of organic-nitrogen conversion,
their combinations — organic, ammo- In some cases it may be desirable to
nium, or nitrate. supply nitrogen in the mix in the nitrate
Organic forms are desirable from the form. This can be done by using any one
standpoint of providing slowly available of several materials; typical sources are
nitrogen over an extended period of time, calcium nitrate, potassium nitrate, and
perhaps making it unnecessary to apply sodium nitrate. Each of these sources
additional nitrogen during the period of must necessarily involve the addition of
release. The rate of breakdown is de- another element. Since potassium must
pendent upon many factors, such as be added anyway, the obvious choice is
temperature, type and population of soil potassium nitrate. Because the amount to
organisms (sees. 7 and 14), nature of be added is small in relation to the bulk
material supplied, and type of soil treat- of the mix, it is frequently good pro-
ment. For a full explanation of the bases cedure to dissolve the salt in water and
for selection of materials and methods sprinkle this solution over the soil before
of use see Section 7. Since the use of too or during mixing.
much of these materials may result in Another procedure sometimes used is
poor plant development, it is desirable to omit all nitrogen sources from the mix
to make trial runs for each major crop and then start a program of liquid or dry
before deciding the amount to be in- surface feeding immediately after plant-
eluded. Once the organic nitrogen has ing. Such a program might consist of
been added to the soil, breakdown be- liquid feeding with a solution made up
[105]
of some soluble nitrogen source such as
calcium nitrate, ammonium nitrate, am-
monium sulfate, or urea (Sec. 5). Dry
application to the soil surface of hoof
and horn or blood meal might be used
instead of a liquid source.
Phosphorus
Of the several sources of available
phosphorus, those which best suit the
purpose here are known as superphos-
phates. There are two principal grades,
both made from phosphate rock and both
supplying readily available phosphorus
with a low salinity effect. They are
known as single superphosphate (18 to
20 per cent available P205) and double
superphosphate, also known as treble or
triple superphosphate (40 to 50 per cent
available P205) . These are monocalcium
phosphates, the former containing extra
calcium in the form of gypsum.
Potassium
As indicated above, this element can
be supplied in the form of potassium
nitrate (46 to 48 per cent K20). Other
sources are potassium sulfate (50 per
cent K20) and potassium chloride (60
per cent K20) .
All sources of this element currently
in common use are completely water-
soluble and must be used with care, as
they add directly to the soluble salts of
the soil mix. The sulfate form is most
frequently used, the sulfur fraction also
being a plant nutrient. A slowly available
form of potassium would be an ad-
vantage. Glass frits containing 12 and 20
per cent potash prepared by the Ferro
Corporation, Cleveland, Ohio, were used
experimentally by the Department of
Plant Pathology and R. H. Sciaroni in
1951-52. Manufacturing difficulties kept
this product ofT the market. A 35 per cent
potassium frit (Dura-K) has recently be-
come available.
Lime
Almost any proportions of the fine
sand and peat moss will result in a
medium which is acid in reaction. The
fine sand usually will have very little
buffering capacity, even if it is alkaline
in reaction. The highly acid peat moss
has a high buffering capacity and will
be a predominant factor in the final pH
reaction. A desirable pH range for the
growth of most green plants is between
5.5 and 6.5. The pH of peat moss is nor-
mally in the vicinity of 4.0. In order to
partially neutralize the acidity, it is neces-
sary to add some form of lime. Calcium
carbonate or oystershell lime are typical
of acceptable materials which will supply
calcium and also neutralize the acidity.
Dolomite lime is a natural form of cal-
cium and magnesium carbonate, which
supplies two elements important to plant
growth, calcium and magnesium, and
which also provides the necessary neu-
tralizing effect.
Some fine sand sources may possibly
contain lime, and in such cases the lime
addition to the mix should be adjusted
for this. Otherwise the final reaction of
the mix might be high enough to result
in some micronutrient-deficiency symp-
toms in sensitive plants. Because such
a situation is rare, the recommendations
are based on the assumption that no lime
is present.
The calcium and magnesium addition
may be important in cases where irriga-
tion water is either extremely low in
salinity or where it is soft owing to a
high sodium percentage. If extra calcium
is considered desirable, it may be sup-
plied as gypsum without affecting soil re-
action. Where waters are hard, but low
in sodium percentage, there is little
danger of deficiency of calcium and
magnesium.
Micronutrients
Mineral elements necessary to plant
growth and development include those
previously mentioned (nitrogen, phos-
phorus, potassium, calcium, magnesium,
sulfur) plus certain others (zinc, manga-
nese, iron, boron, molybdenum, copper)
which are termed "micronutrients" be-
I L06 |
cause their presence is necessary in only
minute amounts. In fact, they can be
quite toxic to plants if present in more
than a few parts per million parts of soil.
The fact that they are required in such
minute amounts and are natural compo-
nents of peat, soil, fertilizers, and water
makes it improbable that a soil mix will
have a deficiency of a minor element.
Investigations to date have shown no
benefit from micronutrient additions to
the U. C. soil mixes, except in special
cases such as the following. It has become
standard practice in growing certain
crops to apply some of the chelated iron
products during certain periods of the
year, usually winter. Azaleas, gardenias,
roses, Liquidambar, heather, and sanse-
vieria are examples of crops commonly
receiving this type of treatment in Cali-
fornia nurseries. Frequently the iron-
chlorosis pattern on the foliage is due to
root disease (Sec. 3), excess fertilizer,
or excess lime, and can therefore be
eliminated by the use of soil mixes and
handling procedures outlined in this pub-
lication. Until further investigations in-
dicate some benefit from micronutrient
additions, no general recommendation
for their use is made.
[107]
SECTION
Nitrogen in
Nursery Soils
O. A. Matkin
Philip A. Chandler
Types of nitrogen
The ideal soil mix
Tests with nitrogen in the U.C. soil mixes
Factors affecting nitrogen release from organic sources
Surface application versus mixing
Adjusting to specific situations
lthough NO one essential nutrient
is more important than any other to
plants, certain elements assume greater
importance because of practical limita-
tion of supply. Nitrogen, phosphorus,
and potassium receive the most attention
in the average fertilizer program. Of
these three, nitrogen is most complex in
form and behavior in both soil and plant.
In the average nursery or greenhouse op-
eration, adequate control of nitrogen
availability constitutes the major fertil-
izer problem.
TYPES OF NITROGEN
For purposes of this section, nitrogen
may be considered as existing in three
general forms.
Organic nitrogen
Organic nitrogen is generally unavail-
able for plant use. An important excep-
tion is urea, which is organic but for all
practical purposes acts like an inorganic
Urea and urea-formaldehyde fertilizers
may contain biuret, a by-product toxic
to many plants. Unless labeled biuret-
free, these materials should be used only
after thorough testing on each crop.
form. Organic nitrogen is linked to
carbon and is not normally water-
soluble. Certain organic forms such as
the amino acids (structural components
of the proteins) have been shown to be
absorbed by plant roots, but their oc-
currence and importance in the nursery
soil is minor.
Insoluble organic nitrogen might be
considered as a storage form; available
nitrogen will be produced from it by
chemical or microorganism activity.
Sometimes, as in manures or leaf molds,
steaming will result in a chemical reac-
tion which produces an available form.
The more stable organics will require ac-
0
tion by microorganisms to produce this
available nitrogen.
Ammonium nitrogen
The first breakdown product of or-
ganic nitrogen which is of practical in-
terest to the nurseryman is ammonium.
This ammonium nitrogen may also be
provided as a commercial fertilizer, such
as ammonium sulfate or dissolved am-
monia. Urea is quickly hydrolyzed in
the soil to produce the ammonium form.
Ammonium nitrogen is water-soluble,
can be absorbed readily by the roots, and
can be utilized by the plant. In certain
cases utilization may be so fast as to dis-
rupt normal functioning of the plant. Al-
though water-soluble, the ammonium
form of nitrogen is not as readily leached
through the soil as is nitrate. Because of
the positive charge of the ammonium ion
it may be removed from solution by the
negatively charged clay and organic in-
gredients; this prevents its being leached
from the soil. Nitrate, which is negatively
charged, may be readily leached. This
nonmobile status of ammonium is tem-
porary, owing to its subsequent conver-
sion to nitrate. Also, the presence of
other positively charged ions (for ex-
ample, calcium, magnesium, sodium, and
potassium) may cause the ammonium to
be "unseated" and released into the soil
solution, which makes it leachable. It is
evident from the foregoing that am-
monium nitrogen applied to the soil sur-
face may not reach the root zone with
the first irrigation. For this reason it is
sometimes referred to as being more
slowly available than the nitrate form,
whereas it is just as available as nitrate
if it is in the vicinity of the root.
Nitrate nitrogen
The conversion of ammonium nitrogen
to nitrate nitrogen is also by microor-
ganisms (Sec. 14). Nitrate is completely
water-soluble and, since it is negatively
charged, it does not enter into any non-
mobile combinations with soil compo-
nents. In a normal well-aerated soil,
nitrate is, from a practical viewpoint,
the end product of nitrogen conversions.
Under prolonged conditions of compost-
ing of organic products, most of the
nitrogen will be converted to the nitrate
form. In the field little ammonium nor-
mally exists except under very acid or
waterlogged conditions, the organic ni-
trogen being slowly converted to am-
monium and then relatively rapidly to
nitrate. Under the natural conditions
where plants evolved, nitrate was, there-
fore, the principal form of nitrogen
utilized. Perhaps some plants have lost
their tolerance to ammonium as a result.
The cycle of nitrogen within the plant
is the opposite of that in the soil. Nitrate
is slowly converted to ammonium, which
is rapidly combined with certain or-
ganic compounds to form proteins, en-
zymes, pigments, and many other com-
plex substances. Under natural condi-
tions, ammonium nitrogen and its first
reaction products will not be present
within the plant in appreciable quan-
tities. Under artificial conditions, if am-
monium nitrogen is supplied directly, an
abnormal accumulation of ammonium
and initial reaction products may occur
within the plant, resulting in possible
"self-poisoning." An important concern
of this section is this ammonium toxicity
and its prevention.
THE IDEAL SOIL MIX
The perfect soil mix would not only conditions during plant growth. This
have the desired physical properties but state would presumably be provided by
would also maintain optimum chemical incorporating in the mix, sources of ni-
[109]
trogen, phosphorus, potassium, and the
other elements, so that an optimum
amount would be available for initial
plant growth. As plant growth and leach-
ing reduced the available nutrients they
would be supplied by breakdown of some
insoluble storage form. The U. C.-type
soil mixes have been an effort to ap-
proach this ideal as closely as is prac-
ticable. To provide an indefinite period
of optimum fertility under a variety of
growing conditions is impossible with
present knowledge and materials. The
first compromise must, therefore, be to
provide a limited period of optimum fer-
tility and rely on customary procedures
of fertilization to extend the useful fer-
tility of the mix. In the case of most ele-
ments this is readily accomplished; phos-
phorus, potassium, calcium, and magne-
sium can be supplied (Sec. 5), and they
will remain in adequate supply for a con-
siderable period of time. The micro-
nutrients seem to be supplied by the raw
materials of a U. C.-type mix (Sec. 6).
The principal problem is that of the
nitrogen supply. The insoluble and initi-
ally unavailable organic form of nitro-
gen offers an opportunity to provide the
desired reservoir. The addition of a
small amount of initially soluble nitro-
gen (for example, as nitrate from po-
tassium nitrate) would seem to satisfy
the requirements.
TESTS WITH NITROGEN IN THE U. C. SOIL MIXES
Seldom can a procedure or theory be
developed for general practical use by
research confined to the laboratory. The
U. C.-type soil mixes were no exception.
Procedures which seemed to work
out very satisfactorily in the Department
of Plant Pathology glasshouses some-
times failed in nurseries. In the process
of development, advantage was taken of
these failures to determine the shortcom-
ings both of the mixes and of the aver-
age nursery. Some of the problems en-
countered were related to the physical
aspects of the medium and, as a result of
information gained from their study,
rather definite specifications have been
outlined in Section 6. Fertility problems
seemed to be related primarily to the
quantity and form of nitrogen present.
Our first attempts to provide a stand-
ard formula for fertilizer additions fol-
lowed the important contributions of the
John Innes Horticultural Institution in
that the only nitrogen addition was hoof
and horn meal. This material would pro-
\ ide a continuous supply of nitrogen that
mi^'lit almost match the progressively in-
creasing requirements of the growing
plant. Initial trials indicated that this
procedure did work quite well. The John
Innes rates of organic nitrogen were in-
creased substantially, which resulted in
improved plant growth; this was because
the fine sand is much lower in nitrogen
than the composted turf loam used by
the Institution.
The resulting procedures were adopted
by a few growers who were having dif-
ficulties with compost-type mixes. Most
of these growers produced bedding
plants, excellent crops for testing a soil-
mix procedure because the plants are in
the most sensitive stage of development,
and results are quickly evident. There-
fore, most of the studies reported in this
section were conducted on bedding-
plant problems.
Relatively few growers were treating
their soils for disease control at this
time, and the first results were very en-
couraging. However, several shortcom-
ings soon became apparent. First, disease
still frequently wiped out substantial
portions of the crop; second, initial
growth of the transplanted seedlings was
not always as rapid as was observed in
[110]
some of the compost mixes. The first
difficulty could be prevented by treat-
ment of soil, containers, and planting
material, and a sanitation program (sees.
1, 3, and 8 through 13). The standard-
ized system of soil mixes was being de-
veloped to make such treatment simple
and certain. Comparative soil tests sug-
gested that the second problem was re-
lated to available nitrogen supply, and
studies on this were undertaken.
Tests with Starter Solutions
We used two materials, ammonium
sulfate and calcium nitrate, at several
strengths as liquid fertilizers. Seedlings
were transplanted to flats containing soil
mix B with fertilizer V (B) or VI (B)
(Sec. 5) and watered in with these solu-
tions. No subsequent fertilizer was ap-
plied.
The results of these trials indicated
that calcium nitrate at approximately 2
ounces per 5 gallons of water would
greatly enhance the initial growth with
little danger of plant damage. Ammo-
nium sulfate was ineffectual or retard-
ing, and was not used in further tests.
Extensive experiments were conducted
in flats in the glasshouse, using twenty
kinds of bedding plants and vegetables.
Seedlings of fifteen of them (China aster,
tomato, zinnia, stock, Tagetes, pansy,
verbena, phlox, celery, lobelia, pepper,
snapdragon, delphinium, vinca, and
cineraria) had 87 to 100 per cent (aver-
age 97.6 per cent) survival when sup-
plied with ammonium from hoof and
horn meal in high or low amounts —
fertilizers V (B) or VI (B) — with or
without a calcium nitrate starter solu-
tion. Seedlings of clarkia, sweet alyssum,
Iceland poppy, and carnation had poor
survival (0 to 80 per cent; average, 50.3
per cent) when supplied with high or
low amounts of hoof and horn but no
calcium nitrate, as against 47 to 97 per
cent (average, 79.3 per cent) with cal-
cium nitrate. In every instance but one,
growth (fresh weight) was greater when
calcium nitrate was added to either low
or high amounts of hoof and horn.
Growth was superior in half the cases
with low, and half with high amounts
of hoof and horn, with or without cal-
cium nitrate. It was concluded that the
calcium nitrate starter solution was
beneficial to all the plants tested, and
was extremely helpful with a few.
Clarkia, sweet alyssum, and carnation
appeared to be sensitive to ammonium
(exhibiting marked reduction in survival
and growth), and this was partially pre-
vented by the calcium nitrate (fig. 67).
If the plant immediately began rapid
growth it was able to use ammo-
nium, but if it was growing slowly am-
monium seemed to depress growth.
Soon after the above tests were con-
ducted, nursery use of the calcium nitrate
solution was successfully undertaken. It
was a logical deduction that the nitrate
might be supplied in the mix by sub-
stituting potassium nitrate (fertilizers I,
II, III) for the previously used potas-
sium sulfate (fertilizers IV, V, VI). This
procedure was adopted by some nur-
series, and eliminated the starter solu-
tion.
Ammonium Toxicity
The solution of one problem seemed
to lead to another. In certain crops at
times during the year, plant stunting
and loss occurred. Root damage was ob-
served which did not involve a pathogen.
In some crops leaf burning indicated
possible saline conditions. Comparative
soil tests indicated that in only a few
cases was salinity a factor, but that am-
monium was always present in substan-
tial amounts with little or no nitrate
nitrogen. The most severe damage oc-
curred when ammonium was present in
sufficient quantity to produce a saline
condition. In some seed flats, yellowing
of seedlings occurred when ammonium
was the predominant source of nitrogen,
even though present in relatively small
[in]
4tto
Fig. 67. Beneficial effect of a calcium nitrate starter solution on seedlings of stock (above) and
petunia (middle) grown in steamed U. C. soil mix B (25 per cent peat; IVi lb. of hoof and
horn meal per cubic yard). Flats at left received single applications of the solution, those at
the right did not. Ammonium injury, shown by sweet-alyssum seedlings (below, left) grown in
the same mix, was reduced by three applications of calcium nitrate solution (below, right).
amounts (that is, 18 to 20 ppm of dry
soil; sodium acetate extraction). It was
further noted that where plants did not
show injury some were rather soft, light
in color, and grew quite rapidly (for
example, petunia) ; see Section 14 for
explanation of this effect. When plants
were beyond the seedling stage, they
apparentl) were unaffected hy this con-
dition, (/rogan and /ink (1956) have
also recently shown that free ammonia
or ammonium hydroxide may cause
severe injury to roots and tops of lettuce
plants in California fields. Application
of organic nitrogenous fertilizers to cold
waterlogged soil, or the use of aqua or
anhydrous ammonia, produced the in-
jury. Ammonium sulfate, ammonium
nitrate, or calcium nitrate caused rela-
tively little damage.
[112]
Certain bedding plants proved to be
good indicators of the presence of am-
monium. Phlox and verbena suffered
severe leaf burn; carnations, sweet alys-
sum, and stocks lost their roots, and
cotyledons turned yellow. Petunia, on
the other hand, seemed to thrive on
moderate amounts of ammonium, but
when levels became too high, extreme
iron chlorosis developed in the youngest
leaves. Iron chlorosis was also noted on
snapdragon seedlings.
At this point there seemed little doubt
that the problem was related to the
organic nitrogen source and the effect
of soil treatment on the organisms in-
volved in nitrogen conversion (Sec. 14).
The following explanation may enable
the grower to better understand the
principles involved.
Organic nitrogen is converted to the
ammonium form in several steps involv-
ing the activity of certain microorgan-
isms. This group consists of numerous
fungi and bacteria (including spore
formers) .
The conversion of ammonium to
nitrate is a stepwise process involving
heat-susceptible, nonspore-forming bac-
teria, as explained in Section 14. Ob-
viously, any condition which affects the
population or the activity of these organ-
isms will affect the rate of nitrogen re-
lease from the organic, and conversion
from the ammonium form. Treatment of
the soil with steam or chemicals to rid it
of pathogenic fungi and bacteria has a
marked effect on the population of these
organisms as well as many others which
may be present (Sec. 14). In general,
the treatments will reduce the numbers
of the organisms which produce ammo-
nium from organic nitrogen and will
eradicate bacteria which produce nitrate
from ammonium. These facts, which have
been reported by many workers, were
verified in the following experiments
with various treatments of a U. C.-type
mix, followed by inoculation with am-
monifying and nitrifying organisms.
Inoculation tests
In order to determine the effect of
inoculation on nitrogen release, we pre-
pared a soil mix of the U. C. type using
hoof and horn (4% lb. per cu. yd.) as
the source of organic nitrogen, without
any inorganic nitrogen. The mix was
divided into six groups:
1. Not steamed, not inoculated;
2. Not steamed, inoculated;
3. Steamed l/2 hour at 212° F, not
inoculated;
4. Steamed % hour at 212° F, inocu-
lated;
5. Steamed 8 hours at 212° F, not
inoculated;
6. Steamed 8 hours at 212° F, inocu-
lated.
A water suspension of a soil known to
contain ammonium and nitrate-produc-
ing organisms was uniformly mixed with
the soil for series 2, 4, and 6. Series 1, 3,
and 5 were treated with an equivalent
volume of water only. All containers of
soil were stored at 70° F. Precautions
were taken to avoid chance contamina-
tion, and soils were not allowed to dry
and thus inhibit organism activity.
Samples of soil were taken at the start
of the experiment and at 5, 7, 14, 21, and
28 days. These samples were immediately
oven-dried and analyzed for available
ammonium and nitrate nitrogen. A 1:5
soil-water suspension was shaken with an
excess of calcium sulfate for 30 minutes
before filtering and analyzing.
The results are presented graphically
(fig. 68), each graph representing an
average of three replicates. The experi-
ment gave the following results:
1. When reinoculation was prevented,
steaming completely inhibited ni-
trate formation. The nitrifying bac-
teria were completely eradicated by
the treatment.
2. Steaming reduced the rate of am-
monium production but did not
completely inhibit it. Only part of
the ammonium producers were
killed by steaming.
[113]
NOT INOCULATED
INOCULATED
200"
100-
8 0
-
Not stea
med
NH +
4
N03 /
•
A
s
-
— -»_
I
HOKy
s
1
1
Not steamed
NH. + NO
200
£
Q.
Q.
O)
o
0-1-
Stea med Vi hr.
NH + NO
Steamed Vi hr.
NH + NO,
4 •»■
NO3 /
3 /
,<r
J> 200
_g
'5
>
<
100-
Steamed 8 hrs.
NH + NO
10
20
Time (days)
7o
Steamed 8 hrs.
NH4+NQ3
NOa/
,-^
10
Time (days)
20"
7o
Fig. 68. Ammonium and nitrate nitrogen production in steamed and unsteamed U.C.-type soil j
mix, with and without inoculation by nitrogen-converting organisms, held at 70°F. The figures
represent an average of three series. See p. 113 and 115 for explanation.
[ 114]
3. There was no significant difference
between the effect of V2" and 3-hour
steaming on organisms which pro-
duce ammonium and nitrate from
the organic nitrogen. The treatment
intervals inhibited activity to about
the same degree.
4. Inoculation reestablished the ni-
trate-producing power of the soil,
but nitrification was delayed for
about 10 days. The nitrate produc-
tion in the unsteamed soil was also
enhanced by inoculation, indicating
that the fine-sand subsoil used was
low in nitrifying bacteria.
5. Inoculation enhanced ammonium
production in all cases, but did so
to a lesser extent in the unsteamed
soils.
In the nursery, nitrate is produced in
a steamed soil as a result of accidental
inoculation. Since ammonifiers are both
numerous and of many types they are
better able to reestablish under a variety
of conditions than the nitrifiers (Sec.
14). If inoculation is to be used as a
means of reducing ammonium toxicity,
it will be desirable to exclude ammo-
nium-producing organisms from the
inoculum. Otherwise the enhanced am-
monium production could defeat the
purpose of the inoculation.
A steamed soil will normally become
reinoculated with nitrate-forming bac-
teria in a few days to a few weeks. When
plants are sensitive to ammonium, and
conditions are favorable for its accumu-
lation, procedures must be adopted that
will avoid damage. At present the pos-
sibility of artificial inoculation with
nitrifying bacteria is insufficiently ex-
plored to be practically useful. Presently
the only other approach is to control am-
monium production by adjusting the
amount and type of organic nitrogen
used in relation to the conditions which
affect its rate of release. To compare the
rate of breakdown of different organic
nitrogens under a variety of treatment
and environmental conditions, another
series of tests was run.
Production of Available Nitrogen
from Organic Sources
The experiment was designed to de-
termine the effects of different forms of
organic nitrogen, rate of addition, steam-
ing, and storage temperature of the soil
mix upon release of available nitrogen.
Organic nitrogen sources were:
1. Castor pomace (5.75 per cent nitro-
gen) ;
2. Cottonseed meal (7 per cent nitro-
gen) ;
3. Fish meal (11 per cent nitrogen) ;
4. Blood meal (13 per cent nitrogen) ;
5. Hoof and horn meal (13 per cent
nitrogen) ;
6. Urea-formaldehyde resin (35 per
cent nitrogen) ;
7. Steer manure (2 per cent nitrogen) .
Also included were :
8. Leaf mold in place of peat moss,
without other nitrogen source;
9. Control; peat moss, but no other
organic nitrogen source.
Soil mix B (25 per cent peat) was
used in all except no. 8 above. Potassium,
phosphate, and lime were added to all.
Hoof and horn was added at the rate of
4% and 6% pounds per cubic yard; the
other nitrogen sources were added to
supply the same amount of actual nitro-
gen. One set of samples of each form of
organic nitrogen was steamed (212° F
for 30 min.), another set not steamed,
and both were stored at 50° or 70° F.
Soils were protected from recon-
tamination, and samples taken at 0, 11,
24, 38, 52, 81, 102, 133, and 149 days.
Ammonium and nitrate nitrogen were
determined on each sample, using a 1:5
soil-water extraction ratio in the pres-
ence of excess calcium sulfate.
Effect of treatments on release
of available nitrogen
Three of the above nine series (steer
manure, leaf mold, and the control)
[115]
c
d)
Ui
O
J)
_Q
_D
'5
>
<
STEAMED
NH4+ NO 3
— T—
15
50
Time (days)
NOT STEAMED
NH4 + N03 s"^*'*
//'MO ,
/ I
/ 1
/ t
/ /
/ •
1 1
— i
100
15
50
Time (days)
100
Fig. 69. Diagrams showing general character of the effect of steaming of U.C. mix B on con-
version of organic nitrogen to available forms. See p. 115 and 116 for explanation.
produced little or no nitrogen ; the others
produced substantial amounts. The check
showed little available nitrogen under
any conditions; toward the end of the
experiment there was a slight tendency
for available nitrogen to increase, prob-
ably from the peat moss, which normally
contains about 1 per cent nitrogen. In
the mix containing leaf mold, the avail-
able nitrogen level was higher than in
the control but was affected by treatment
only when the unsteamed mix was
stored at 70° F. In this lot an appreciable
amount of available nitrogen accumu-
lated during five months' storage, but
the amount produced did not compare
with that from nitrogen sources 1
through 6. Steer manure showed some
active release of nitrogen at 70° after
50 days or more. The amount was less
than that released from leaf mold, how-
ever, and is considered to be of little
consequence from a practical standpoint.
Initial tests indicated that the manure
mix was very saline.
Organic nitrogen forms 1 through 6
were sufficiently similar in their pattern
of breakdown to be discussed together.
Two diagrams (fig. 69) show this
general pattern. Whether steamed or not,
nitrogen was more rapidly released dur-
ing the first month than in the next two
months. When the mixtures were un-
steamed, nitrate was produced; but there
was a delay before the rate was sufficient
to prevent ammonium accumulation.
When the mixtures were steamed, no
nitrate was produced in 100 days, in-
dicating that reinoculation by nitrifying
bacteria had not occurred.
In unsteamed soil the time interval
before nitrification began was greatly in-
creased by low temperature and by low
organic nitrogen. The results are sum-
marized in the tabulation below.
One may conclude that these condi-
tions retarded the activity of nitrifying
organisms.
Further indication of the effect of
these factors upon rate of nitrogen re-
lease is shown by the average time re-
quired for available nitrogen to reach 50
Storage temperature
Time required for nitrification to begin (unsteamed soil)
With 4'j lb. rate
With B\-i lb. rate
50 F
70 F
60-130 days, av. 95 days
10-40 days, av. 30 days
60-110 days, av. 88 days
10-25 days, av. 18 days
[116]
Storage temperature
Soil
treatment
Average storage time to reach 50 ppm
of available nitrogen
With VAVa. rate
With SH lb. rate
50° F
f Steamed
\ Unsteamed
f Steamed
\ Unsteamed
37 days
27 days
18 days
16 days
28 days
19 days
12 days
10 days
70° F
ppm of dry soil, a moderate supply for
plant growth in soil mix B; the data are
summarized above.
An increase in the storage temperature
resulted in an increase in the rate of
available-nitrogen production. Increas-
ing the amount of source material also
increased this rate. On the other hand,
steaming had a retarding effect. The rate
of release of available nitrogen was re-
duced by steaming the soil, by low
storage temperature, and by low rate of
addition of organic nitrogen. These con-
ditions evidently retarded the activity of
organisms producing ammonium nitro-
gen from organic sources.
At the time of the first sampling (11
days) there was, in this expsriment, an
appreciable increase in the ammonium
concentration in all but the steamed soils
stored at 50° F. In these, ammonium
production was only slight, except for
urea-formaldehyde, to be discussed
later. In the previously described (fig.
68) experiments on inoculation, ammo-
nium production was appreciable at 5
days. It seems that if the temperature is
high enough, activity of ammonifiers be-
gins very quickly, certainly within a few
days. Still another indication of the in-
fluence of these environmental conditions
on rate of nitrogen release is shown by
the concentration of available nitrogen
at given times in the soil mix; the data
are given in table 11.
Again, the rate of release of available
nitrogen was reduced by steaming, low
storage temperatures, and low rate of
nitrogen addition. In all cases the
amount of available nitrogen evolved
Table 1 1 . Effect of Storage Interval on Concentration of Available
Nitrogen in Soil Mix
Average of six organic nitrogen sources
Storage temperature, °F
Treatment
Concentration of available nitrogen,* in ppm of dry soil
With \y2 lb. ratef
With 6% lb. ratet
15
days
50
days
100
days
15
days
50
days
100
days
50
f Steamed
(Unsteamed
{ Steamed
\ Unsteamed
20
33
45
61
74
86
80
120
80
96
95
159
33
52
63
83
88
94
108
180
96
126
108
214
70
* Average of total available (ammonium plus nitrate) nitrogen from organic nitrogen sources 1 through 6.
t Hoof and horn meal added at 4'2 and 612 pounds per cubic yard. Other nitrogen sources were added
to supply an equivalent amount of nitrogen.
[117]
was substantially greater in the first than
in the second 50-day period. This ten-
dency for leveling-off was greater in
steamed than in unsteamed soil, as
shown in figure 69.
Nitrogen supplied by
specific materials
There were marked differences be-
tween the available nitrogen released
from the six different organic sources
(table 12).
The materials (castor pomace, cotton-
seed meal, and fish meal) that most
rapidly produced available nitrogen,
were, surprisingly enough, those with the
lowest original nitrogen content. Of the
three, castor pomace seemed to break
down most rapidly. Blood meal, hoof
and horn meal, and urea-formaldehyde
all have a much lower rate of release of
available nitrogen, and the values are
considerably lower than those of the first
three.
Steaming enhances the breakdown of
urea-formaldehyde, whereas the effect
was just the opposite in all other mate-
rials. In the more complete data it is
apparent that there was an immediate
build-up of ammonium whenever the
urea-formaldehyde mix was steamed.
Possibly the effect of steaming was to
partially hydrolyze the compound to pro-
duce some free urea, which was quickly
converted to ammonium. After this first
surge, the rate of nitrogen release was
very slow. In all cases where the mixes
were not steamed, the rate of release was
slower from urea-formaldehyde than
from any of the others. Thus, urea-for-
maldehyde has certain desirable prop-
erties, but a serious drawback of initially
releasing ammonium when steamed.
As a result of these tests the materials
might be listed in the descending order
of their activity as follows: castor
pomace; fish meal; cottonseed meal;
blood meal and hoof and horn (equal) ;
urea-formaldehyde.
This information does not necessarily
Table 12. Available Nitrogen Released by Various Organic Nitrogen
Sources in a Soil Mix After 30 Days' Storage
Two rates of organic application, steamed and unsteamed, and stored at two
temperatures
Storage
temperature,
op
Treatment
Rate,
lb. per
cu. yd.f
Concentration of available nitrogen,* in ppm
Castor
pomace
Cotton-
seed
meal
Fish
meal
Blood
meal
Hoof
and
horn
meal
Urea-
formal-
dehyde
resin
50
<
Steamed
Unsteamed
Steamed
Unsteamed
UA
Wa
Wa
Wa
Wa
Wa
Wa
Wa
60
100
93
128
73
132
160
160
54
75
108
116
60
98
95
140
60
92
80
130
66
114
104
160
25
48
47
60
45
60
63
105
25
37
47
63
50
60
70
95
80
73
42
46
78
64
60
64
70
Average steame
d
91
130
72
115
83
119
45
69
43
69
74
53
Average unstea]
ned.
* Total available nitrogen (ammonium plus nitrate) in ppm of dry soil. In steamed (212° F for 30 min.)
series all nitrogen was ammonium.
t Nitrogen addition equivalent to 41 £ lb. or 61 jj lb. hoof and horn meal per cu. yd.
hold when these fertilizers are applied
broadcast or as top dressings (see "Sur-
face Application versus Mixing," below) .
Hoof and horn meal and blood meal
constitute the most desirable sources of
organic nitrogen for the soil mix, in that
they are slower in their release of avail-
able nitrogen than are castor pomace,
cottonseed meal, and fish meal. If the
problem of initial ammonium release
upon steaming can be overcome or mini-
mized, urea-formaldehyde might be
superior to any of the natural sources —
assuming, of course, that biuret toxicity
can be avoided (Sec. 5).
Until further investigations are carried
out, the effects of thorough chemical
treatment must be assumed to produce
results similar to those found where
steaming was used. Since heat is prob-
ably a major factor in the hydrolysis of
the urea-formaldehyde, chemical treat-
ment might prevent the rapid breakdown
to ammonium by this material.
Application of This Information
Bedding plants
Identification and clarification of the
problems discussed above led to certain
changes in bedding-plant procedure. The
use of organic nitrogen in the mixes was
greatly reduced or eliminated. This re-
duction in nitrogen supply was offset by
the use of nitrate forms. Calcium nitrate
solution was used as a liquid supplement
and in many instances potassium nitrate
has been substituted for potassium sul-
fate in the mix. In addition, hoof and
horn or blood meal was applied as a top
dressing, this procedure supplying
slowly available nitrogen over an ex-
tended period without the dangers of
ammonium toxicity (see "Surface Appli-
cation versus Mixing," below). It was
especially important to avoid large
amounts of organic nitrogen in the mix
during periods of hot weather.
Pot plants
While the work with bedding-plant
growers was progressing, attention was
given to similar problems in greenhouse-
pot and nursery-can culture. In pot-plant
growing the only period of high sen-
sitivity seemed to be in the early growth
of rooted cuttings or small seedlings.
Where plants were vigorous, there was
seldom any setback if reasonable
amounts of organic nitrogen were used.
No problems developed where plants
were moved up from a smaller to a larger
container. There are two primary
reasons for the increased safety in "pot-
ting-on":
1. The amount of soil used for each
plant is substantially less in proportion
to plant size than when potting seedlings
or rooted cuttings with no root ball. The
established plant will require much more
nitrogen and must get it from a relatively
smaller amount of added soil.
2. The root ball which is placed in the
new soil has had time to become reinocu-
lated with nitrifying bacteria. The added
soil will, therefore, become quickly
inoculated and nitrate will be produced.
In some cases, growers are practicing
subirrigation for such crops as Saint-
paulia. In this procedure there is almost
no leaching action and the added nitro-
gen is not so readily lost as with surface
watering. Under these conditions the
upper limit of added hoof and horn has
been about 2% pounds per cubic yard of
soil.
Nursery-can culture
In nursery-can growing the problems
are similar to those encountered in the
bedding-plant industry. Rooted cuttings
or small liners are transplanted into gal-
lon cans where growth of many items
may be relatively slow. This provides
ample opportunity for added organic
nitrogen to supply an excess of available
nitrogen. Although no indications of
specific toxicity due to ammonium have
[119]
been noticed, there have been instances
where the build-up of nitrogen was suf-
ficient to produce a salinity effect. For
this reason organic nitrogen is com-
monly omitted or used in relatively small
amounts. Another reason for reducing
the organic nitrogen is that soils are fre-
quently prepared ahead of time and held
for several weeks to several months be-
fore planting (Sec. 5).
Bed or bench culture
When crops are grown for several
seasons or years in beds or benches, or-
ganic nitrogen may be completely
omitted in the mix and a program of
fertilizing, with or without organic nitro-
gen, followed from the start. There is
little advantage in delaying the initiation
of the long-term program by initial mix-
ing of organic nitrogen into the soil.
FACTORS AFFECTING NITROGEN RELEASE
FROM ORGANIC SOURCES
In well-aerated soils such as those ob-
tained in the physical medium of the
U. C.-type mix, the following factors may
affect the amount and rate of release of
available nitrogen from the organic
form.
Microorganism population
In natural soils the population of
microorganisms will be much higher in
the surface 6 to 12 inches than at greater
depths. Subsoils are frequently low in
organism population. This is to be ex-
pected since the moisture, air, and or-
ganic matter necessary for most organ-
ism activity are more available in surface
soils. The difference in the effect on rate
of nitrogen release by untreated surface
and subsoils may be substantial.
Where heat or chemical treatment is
practiced, the difference between surface
and subsoils is reduced, since all nitrify-
ing bacteria are killed and the population
of those which produce ammonium is
initially reduced (Sec. 14).
Heat and chemical treatment
As suggested in the preceding para-
graph, the procedure of treating the soil
to rid it of pathogens necessarily affects
the whole microorganism population.
Nitrifying bacteria will be eradicated
where treatmenl is effective. Ammonium
production may be reduced but not en-
tirely eliminated. Furthermore, ammo-
nifiers will more rapidly repopulate the
soil. Thus ammonium may be produced,
but not converted to nitrate, until the soil
becomes reinoculated with nitrifiers.
Under normal conditions, inoculation
will occur within a period of several days
to several weeks. This is an uncertainty
which in the future may be eliminated
by the use of inoculation cultures.
Soil reaction (pH)
Highly acid media generally have little
effect on the activity of ammonium pro-
ducers, while inhibiting the activity of
nitrifiers (Sec. 14). This was shown in
a nursery test in which azaleas were
grown in beds of pure peat plus organic
nitrogen. Hydrated lime was worked into
a test bed before planting. After several
months, plants in the limed area were
noted to be darker in color than the re-
mainder. Tests of the growing medium
showed the differences in acidity and
nitrogen concentration as tabulated on
page 121.
It has been demonstrated by Tied j ens
and Robbins (1931) that some crop
plants are unable to utilize the ammo-
nium form of nitrogen when the pH is
low, but do so readily when the pH is in
the neutral to alkaline range. The use of
lime in recommended mixes should de-
crease difficulties of this nature.
[120]
Test bed
PH
Nitrate nitrogen,
ppm of dry peat
Ammonium nitro-
gen, ppm of
dry peat
Limed
Nonlimed
5.9
3.9
350
26
155
225
Soil temperature
In general, the warmer the soil, the
greater will be the activity of micro-
organisms in it. There is an upper limit,
of course, beyond which an increase in
temperature will reduce and even kill
them. When temperatures are low, ac-
tivity is reduced. The nitrifiers are more
critically affected than are the ammoni-
fiers (Sec. 14) . Thus during cool weather
there will be a reduced rate of ammo-
nium production, and an even greater
reduction in the rate of nitrification.
When soil temperatures are below 40° F,
applications of blood meal or other
organic sources may be quite ineffective
and the rate of release of nitrogen too
slow to meet the plant requirements.
Under these conditions the grower
should use soluble materials such as
calcium nitrate.
Concentration and source
of organic nitrogen
As already shown, an increase in
amount of organic nitrogen added to a
soil mix will increase the rate of release
as well as the total amount of available
nitrogen. Therefore, the higher rate of
addition does not necessarily mean that
the period of release will be lengthened.
The sources of organic nitrogen are
quite varied in chemical composition.
Some organic sources of nitrogen seem
to be more readily assimilated by organ-
isms which decompose them than do
others. Urea- formaldehyde, hoof and
horn meal, and blood meal are among
the slowly decomposable forms of or-
ganic nitrogen. Cottonseed meal, castor
pomace, and fish meal are quite rapidly
decomposed. Since the primary objective
in adding an organic nitrogen source to
the mix is one of prolonging the period
of release of available nitrogen, it is most
reasonable to add those sources which
are slowest in rate of breakdown.
As explained below, there are substan-
tial differences in rate of release of avail-
able nitrogen when organic materials
are broadcast over the surface of the soil
as compared with being mixed into it.
Presumably the more finely divided and
more "palatable" materials would result
in more rapid release of available nitro-
gen with surface application.
Moisture and aeration
A soil that is dry will not support
plant growth and, as might be expected,
will retard microorganism activity. It is,
however, unsafe to assume that a stored
soil mix is dry enough to prevent the re-
lease of available nitrogen from organic
sources. In some cases oven-dried and
stored samples have been found to pro-
duce available nitrogen. Lack of ade-
quate moisture would probably be more
damaging to the growing plant than any
side-effect it might have on nitrogen
relations.
Lack of oxygen supply (aeration) is
an inhibiting factor in plant growth and
alters microorganism activity. It has
commonly been accepted that poor aera-
tion will result in nitrite accumulation
(Sec. 14) . It now seems that many of the
troubles blamed on nitrite may have
been due to ammonium toxicity and
salinity. There is recent evidence ( Duis-
berg and Buehrer, 1954) that nitrite
toxicity may have been highly overrated.
In any event, a U. C.-type soil mix pro-
vides a medium with excellent aeration,
and chemically stable to soil treatment.
Nitrite accumulation has thus far not
been found to occur in it.
[121]
SURFACE APPLICATION VERSUS MIXING
Surface application of organic nitro-
gen can be substantially less dangerous
from the ammonium-toxicity standpoint
than when it is mixed into the soil mass.
This greater safety results from:
1. The slower production of available
nitrogen at the surface, owing to
less intimate contact with the soil
mass and to environmental condi-
tions intermittently unfavorable to
soil organisms.
2. The restricted ability of ammonium
to move through the soil into the
root zone (see "Ammonium nitro-
gen," above) .
3. More rapid inoculation with nitri-
fiers at the surface of treated soil,
converting to nitrate the ammonium
produced. Since top-dressing mate-
rials are usually not treated with
heat or chemicals, they may have a
better balance between ammonify-
ing and nitrifying microorganisms.
The restrictions on the use of organic
nitrogen in the soil mass discussed in this
section do not necessarily apply to their
use as surface dressings.
Features of surface application that
are less desirable than soil-mix inclusion
are:
1. Practical inability to make uniform
application ;
2. Danger of plant damage from rapid
decomposition at high temperatures
in contact with the seedling ;
3. Objectionable residues, odors, and
flies.
Under some circumstances it is better
to mix the organic nitrogen into the soil
than to apply it as a later top dressing.
The dangers discussed in this section
from mixing organic nitrogen into the
soil mass encourage cautious and judi-
cious use of it in this way. On the other
hand, there are also problems in using
the materials in surface application.
ADJUSTING TO SPECIFIC SITUATIONS
A grower is never relieved of the
necessity of thinking by this or any other
system of soils and fertilizers. The fore-
going discussion illustrates the complex-
ities of nitrogen application in plant
growing. The problem of ammonium
toxicity is an important consideration
where organic forms are used, but they
may greatly prolong the usefulness of the
soil mix and prevent the occurrence of
extreme nitrogen deficiency. In some
growing operations (for example, pot
plants) organic nitrogen included in the
mix reduces labor and variability from
top-dressing application. Where the U. C.
system is carefully followed the only
nutritional problems which can develop
in the first several months of use must be
related to nitrogen supply. It is im-
portant whether nitrogen is supplied as
ammonium or nitrate, and in what quan-
tity. The information in this section
should aid in crop programming and
analysis of nitrogen nutrition problems.
r 122 ]
SECTION
Heat Treatment
of Soil
Kenneth F. Baker
Chester N. Roistacher
Comparison of commonly used treatments
Benefits from heat treatment of soil
Sanitary precautions in soil treatments
Treatment temperature and time
The form of steam used
Efficient soil steaming
Volume of steam required
Preparing soil for steaming
Uneven heating
Cooling the treated soil
Water content after steaming
Steam-treating home yards
Cost of steaming soil
.HE soil AND the host plant are the two
ultimate sources of organisms that cause
plant disease. Pathogens may be eradi-
cated from the soil by treatment with
heat (this section and sees. 9 and 10)
or chemicals (Sec. 11), and from the
planting stock (Sec. 13) and containers
(Sec. 12) in various ways. These prac-
tices, along with the use of a U. C.-type
soil mix (sees. 5, 6, and 7) and sanitary
practices (sees. 1, 3, and 14). are the
supports for economic modern plant
production through the U. C. system
(frontispiece).
COMPARISON OF COMMONLY USED TREATMENTS
Heat treatment of soil may be done
with steam, a dry source of heat, or hot
water. Each has its place in nursery prac-
tice, the same as chemical treatment.
Steam versus chemicals
The comparative advantages of steam
and the two most commonly used chemi-
cals are shown in table 13. Treatment
[123]
Table 1 3. Comparative Advantages of Steam and Chemical Treatments
of Soil in Common Use in California Nurseries
Characteristic
Steam, 180°-212° F
for 30 min.
Methyl bromide,
4 lb. per 100 cu. ft.
Chloropicrin,
5 cc per cu. ft.
Time required for
treatment
About 1 hr.
24-48 hr.
2-3 days
Time between treat-
ment and planting . .
About 1-2 hr. to cool
24-48 hr.
7-10 days
Kills all pathogens,
weeds, and insects?.
Yes, best treatment;
a few weeds sur-
vive
Most, but not Ver-
ticillium; a few
weeds survive
Yes ; a few weeds
survive
When can penetration
of material be deter-
mined, as a measure
of effectiveness? ....
At once, by measur-
ing soil tempera-
ture
Later, by noting re-
duction of disease
or pathogen
Later, by noting re-
duction of disease
or pathogen
Toxic after-effect to
crops?
None with U.C.-
type soil mixes
Yes, for carnations
and some others
None, when properly
aerated
Use near living plants?
Yes
Within 3 ft. if ade-
quately ventilated
Only with excellent
ventilation
Destroys organisms in
unrotted crop refuse?
Yes
Yes
Poorly
Can it be used any-
where?
Only if portable
boiler used
Yes
Yes
Is its use limited by
environment?
Time and cost in-
crease with cold
or wet soil, but
can be so used
Not recommended
below 60° F
Dosage increased if
soil below 65° F
or wet
Ease of application ....
Easy
Easy
Obnoxious and time
consuming
Dangerous to work-
men?
No
Yes
Yes
Is large capital outlay
required?
If boiler unavailable
No
No
Cost per cu. ft. of soil,
exclusive of labor . .
Less than 2 cents,
including equip-
ment cost
About 2.9-3.2 cents,
excluding equip-
ment cost
About 1.9-3.0 cents,
excluding equip-
ment cost
[124]
with steam is faster, easier, cheaper, and
more effective than with these materials.
It remains the best general method of
disinfesting soil, destroying fungi, bac-
teria, nematodes, weeds, and insects. It
is the standard for judging new chemical
treatments. For these reasons it is the
treatment emphasized in this section.
Steam offers further advantages. It is
more dependable and its effectiveness is
more readily determined than most
chemical treatments. The penetration of
steam can be quickly and easily assessed
by measuring temperature and time. This
is so dependable a measure of effective-
ness that temperature is practically used
for its evaluation, instead of the measur-
ing of disease as must be done with
chemicals. Treatment by steam is funda-
mentally a transfer of heat from the
boiler to the soil, and all factors (such
as soil moisture, porosity, volume, and
temperature) affect a single variable, the
temperature, measured by a thermom-
eter. The effectiveness of chemicals is
modified by many of the same factors,
but the result (concentration of active
chemical in the soil) is not readily de-
termined. Thus, it is commercial practice
to judge penetration of a chemical by the
control of pathogens. Practically, this
measurement is only possible weeks or
months later, and by the occurrence of
disease.
Soil may be steamed, furthermore,
within 1 or 2 feet of living plants without
injury to them. This is a distinct advan-
tage in a planted glasshouse, where it
may be necessary to treat a single bench
or a localized area of it. Chemicals can
be used in this way only with excellent
ventilation and even then there is some
risk (Sec. 11) .
There is no hazard from steaming soil
in the headhouse room or other places
where men are working. In closed areas
the heat may be uncomfortable, but no
noxious or dangerous gases are given off.
There have been no complaints from
neighbors when steam has been used,
whereas serious difficulties have some-
times arisen from chemical fumigation.
There are, however, some conditions
where steam is impractical (for example,
large field areas used for low-value
crops), and some where it is initially
expensive (for example, if a boiler must
be purchased). In such cases chemical
treatments are often used (Sec. 11).
Some chemicals are occasionally injected
with steam (Sec. 10, type 26) , and others
are applied as supplements to it (Sec.
id.
Steam versus
other heat treatments
A dry source of heat (for example,
metal heated by a flame or electricity)
may be used for treating soil. One of the
worst disadvantages of this type of heat
is that it is necessary to apply intense
heat (high temperature) in a limited
area in order to impart the required
quantity (B.t.u.). Usually intensity is
high, quantity is small, and distribution
through the soil is poor. Steam, in con-
trast, imparts a large quantity of heat at
low intensity (212° F), and flows
through the soil to the cold area. It is
almost as though successive heat sources
were turned on along the advancing
front as the steam moves forward. One
of the principal advantages of steam is
that the B.t.u. are released at the point
to be heated. Furthermore, there is a
natural ceiling of 212° when soil is
heated by flowing steam. This is a safety
feature shared by no other heat treat-
ment except by hot water.
From these facts it is concluded that
a dry source of heat may be used for
treating soil that moves past the heater.
When handled in this way, satisfactorily
uniform progressive heating of the whole
soil mass results. It should not be used
to treat a stationary soil mass. In con-
trast, steam is most efficiently used for
treating a stationary soil mass. When a
dry source of heat is used with a moving
soil mass, it is necessary to treat con-
[125]
tainers in some other way (sees. 10 and
12).
The principal disadvantage of hot
water, even when boiling (212° F). is
that it releases so much less heat per
pound to the soil than does steam (Sec.
9) . Hence much more of it must be used
to raise the soil temperature to the same
level. Soil may be puddled by such treat-
ment, and the quantity of water draining
from the soil is messy and troublesome,
particularly in glasshouse beds. Hot
water is less efficient and convenient
than steam for treating soil. About the
only compensating advantage is that
salinity is reduced to a low level by the
leaching provided. Hot water is some-
times used for treating propagating
sand (Sec. 10, type 25). It may be used
for leaching of salts from propagating
beds, which may then be steamed. Its use
is decreasing.
BENEFITS FROM HEAT TREATMENT OF SOIL
The primary reason for most soil heat
treatments is the elimination of fungi,
bacteria, and nematodes that cause plant
disease. There are, however, other
benefits.
Heavy soils become more granular,
with improvement of drainage and aera-
tion. Much of the steaming of glasshouse
rose soils in the United States is done for
this purpose, rather than for disease con-
trol. This same effect, however, often
causes trouble for bedding-plant growers
when they begin steaming and do not
properly adjust watering operations,
since the stock may not be kept suffi-
ciently moist. The formation of toxins
from steaming such heavy soils is dis-
cussed in Section 6.
Improvement of plant growth not
definitely associated with elimination of
known disease sometimes occurs. This
may result from increased availability of
nutrients (Sec. 6), change from nitrate
to ammonium nutrition (Sec. 7), or im-
proved physical structure of the soil, but
is often due to a biological change that
may or may not be directly associated
with disease. This corresponds to the
"increased growth response" from chem-
ical treatment of soil (fig. 119; and sees.
11 and 14).
Elimination of weeds is the benefit
from heat or chemical treatment of soil
over which many growers are at first
most enthusiastic, perhaps because of the
spectacular results. Many bedding-plant
growers have stated that this feature
alone pays for the treatment. Since some
have spent 3 to 4 cents a flat for weeding,
this claim is well founded. The practice
of composting, done in part for the
elimination of weeds, is rendered un-
necessary when soil is treated (Sec. 6).
Very few weeds survive heat treatment of
soil (fig. 70 and Sec. 9). and even these
may be largely eliminated if germination
is started by keeping the soil moist for a
few days prior to mixing and treatment.
SANITARY PRECAUTIONS IN SOIL TREATMENTS
To reduce the possibility of infesting treatment. This eliminates handling and
treated soil with pathogens, it should be
h a ndled as little as possible after steam-
ing or oilier trealment. It is desirable,
therefore, to place the soil in the con-
tainers (pots, fiats, cans, benches) before
insures that the containers are ade-
quately disinfested. The fact that soil
trealment in bulk is discussed in this
manual (sees. 10 and 17) does not imply
that it is equally satisfactory. The method
120 |
is given because some nurserymen do
not find it feasible to adapt in-container
treatment to their operations. When bulk
treatment is used, the containers must
be separately treated and special care
taken to avoid contamination before and
during filling operations.
If new cans, flats, and pots are used,
and these have been carefully handled to
prevent contamination after delivery,
there is less reason to treat after filling.
This is also true for new insert unit con-
tainers for flats. If the flats in which they
are placed have been used before, how-
ever, there is still some risk. Further-
more, the possibility of contamination
during the actual filling operation exists,
unnecessarily, in each of these practices.
It is a wise general practice to place
the soil in containers and then to treat
them as a unit.
Mixing of fertilizers or other in-
gredients into the soil after treatment
should be avoided; this may readily be
accomplished with the U. C.-type soil
mixes (sees. 5, 6, and 7).
TREATMENT TEMPERATURE AND TIME
A temperature of 180° F for 30 min-
utes is adequate to free soil of pathogens,
weeds, and insects (fig. 70, and Sec. 9).
For reasons explained in Section 9, heat-
ing cannot be stopped at 180° in some
kinds of equipment. A final temperature
of 180° for 30 minutes is possible and
satisfactory for treatment of a moving
soil mass with either a dry source of heat
or steam, because the rate of movement
and the amount of steam or dry heat ap-
plied can be regulated. If the English
steam-air mixture system (Sec. 9)
should prove generally satisfactory, this
temperature could also be used for steam-
ing a stationary soil mass. With present
methods, however, steam will not heat a
stationary soil mass to less than 212°.
Hence, a final temperature of 212° for
30 minutes is recommended for steam
treatment of soil in containers or in a
stationary bulk mass.
These temperatures take into account
such practical considerations as the re-
duced rate of heat penetration into clods
and pockets of organic material and
Fig. 70. Temperatures necessary to kill path-
ogens and other organisms harmful to plants.
Most of the temperatures indicated here are
for 30-min. exposures under moist conditions.
°F O
212
200
190
180
170
160
150
140
130
120
110
100
M
Few resistant weed seeds
Resistant plant viruses
Most weed seeds
_ All plant pathogenic bacteria
Most plant viruses
.Soil insects
Most plant pathogenic fungi
— Most plant pathogenic bacteria
Worms, slugs, centipedes
~ Gladiolus yellows Fusarium
— Botrytis gray mold
— Rhizoctonia solani
_ Sclerotium rolfsii and Sclerotica sclerotiorum
~ Nematodes
— Water molds
[127]
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212°
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7 US
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IHHUM
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212°
o
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plant residue. The timing should begin
when the coldest point in the soil mass
has reached 180° to 212° F. Usually a
slight steam flow must be maintained
after this time in order to hold the de-
sired temperature for 30 minutes. Equip-
ment for treatment of bulk soil often will
have cold corners at the bottom. These
should be located by trial, and used as
the temperature test points. The worst
cold corners should be eliminated by
fitting the box with triangular pieces of
wood (see Sec. 10, type 4).
Because steam thus moves through the
soil as an advancing front, temperature
rise at a given point is usually quite
sudden under efficient operating condi-
tions (fig. 71 and Sec. 9). Steam con-
denses on the nearest cold soil particles
and does not penetrate farther until it
has heated them to 212° F. For this rea-
son, several thermometers may be placed
Fig. 71. Diagram showing movement of
steam from the orifice (or) in the buried pipe
(p) through a stationary soil mass. Steam ex-
pands as a spheroid with an elongated top.
If the distance of movement (d) above the out-
let is 1, then that below it is approximately Vi,
and that to the sides is Vi to %. An advancing
boundary or zone of condensation (con) sepa-
rates the unheated soil (us) from that at 212°F.
The same unit at the same instant of heating is
shown in end view in A and in bottom view in
B. The shape of the spheroid would be the same
in side view as shown in A. When the steam
from the top pipe reaches the soil surface (ss),
it escapes (es). Steaming should then continue
at a reduced rate of flow (the "trickle finish")
until the cold corners (cc) are heated. The same
unit as in A and B is shown in C a few minutes
later, with nearly all the soil heated to 212°.
The zones do not overlap as the steam flow
continues, but the steam then tends to flow into
the cold corners. Note that the cold corners
are easily eliminated by a triangular piece of
wood (tr) placed in the vertical angle of the
box.
28 I
at varying distances from the steam in-
puts to plot the advancing heat front. Ac-
curate chemical thermometers must be
used, since inexpensive ones are likely
to give inaccurate readings (see Appen-
dix). Convenient pellets called Tempil
Pellets are available (Appendix) that
melt at indicated temperatures from
113° to 250° F or more. A series that
melts at 163°, 188°, 200°, and 213° may
be placed in various parts of the soil
mass; the highest one melted indicates
the highest temperature attained at that
point.
It is safe to heat a U. C.-type soil mix
to 212° F without the soil's becoming
toxic to plants. With these soils it is
better, therefore, to overcook than to
risk incomplete heating. When possible,
other types of soils should be heated to
only 180° until the grower finds that the
particular soil may be safely heated to
212°.
Temperature requirement for
pinto-tag certificates
In August, 1954, the California De-
partment of Agriculture ruled that vege-
table plants grown in flats could be
moved, without inspection at destination,
between counties participating in the
intercounty nursery stock certificate
agreement. To qualify, the soil and flats
must be either "steamed in a closed
chamber until temperature of all soil
reaches 180° F" or treated for 24 hours
with methyl bromide at 4 pounds per
100 cubic feet, and protected from recon-
tamination. The certificate may be used
for shipments by authorized nurseries of
plants so handled. These "pinto-tag" cer-
tificates are becoming recognized as in-
dicative of superior nursery stock.
THE FORM OF STEAM USED
Free-flowing or
pressureless steam
Of the three forms of steam used for
soil treatment, the free-flowing is the
most commonly used and probably, con-
sidering equipment cost, the most prac-
tical. The steam is at atmospheric pres-
sure or very slightly above. This means
that large-diameter, light-weight, quick-
coupling aluminum irrigation pipe can
be used for mains, and that a lighter and
less expensive boiler is possible. There
are other advantages for this type of
steam (sees. 9 and 10). If a boiler must
be purchased for soil steaming, one op-
erating at little or no pressure probably
is the best investment.
Many boilers used for glasshouse
heating deliver steam through the mains
under pressure. When such steam is used
for soil treatment, it drops back to at-
mospheric pressure as it enters the soil.
The steam supplied is slightly drier than
the free-flowing type and carries a little
more heat. Its effect on the organisms is
the same as the free-flowing type, since
they are subject to no pressure.
Steam under pressure
Soil may be subjected to steam at about
15 pounds' pressure in tight containers
(autoclaves or cannery retorts). Al-
though there is about 1.4 per cent more
B.t.u. per pound in this than in free-
flowing steam, there is no real gain in
treatment efficiency (Sec. 9). Steam at
15 pounds' pressure has a temperature
of 249.8° F. Since no worthwhile pur-
pose is served, and the excessive heat
may be detrimental to the soil, the use
of pressure steamers is not recommended.
Furthermore, the increased cost of equip-
ment over the free-flowing tvpe is ap-
preciable.
[129]
Superheated steam
Steam which is heated to 300° F de-
livers only 4.4 per cent more B.t.u. per
pound than does pressureless steam (Sec.
9). It has the advantage of being drier,
but this is insufficient to justify the
greater boiler cost. If the soil is at the
right moisture content before treating,
even free-flowing steam does not leave
the soil too wet for planting. Superheat
boilers are, furthermore, not used for
heating glasshouses.
EFFICIENT SOIL STEAMING
To use steam efficiently, the rate of
flow should be adjusted to the volume of
soil treated, or the volume of soil should
be altered to the steam flow available.
The efficiency of the operation depends
on the proper balancing of all the factors
by the grower.
Balanced steaming and the
trickle finish
There are both upper and lower limits
to the flow rate for efficient use of steam
(fig. 74 and Sec. 9). If the rate is too
high for the volume of soil surrounding
each steam input, the steam will escape
or "blow out" from the surface (if the
input is buried) or escape through open-
ings (if released into a chamber contain-
ing soil) before some of the soil reaches
212° F. Steam will then be wasted. If the
flow rate is too low, the treatment period
will be unduly prolonged, there will
probably be excessive loss of heat from
the soil surfaces before the mass is
heated, and the soil may become too wet.
"Balanced steaming" is achieved by
adjusting soil volume and steam flow to
the range of maximum efficiency (Sec.
9 ) . This range is affected by so many
factors that no definite recommendation
can be made. It can be readily found by
trial for each set of conditions, since
there is a fairly wide acceptable range of
flow rates and input spacing distances.
The rate should be such that the tempera-
ture rise at any point is rapid, once it has
started. The best flow rate approximates,
but remains just below, that which per-
mits steam to escape. When only a small
quantity of soil remains at a temperature
below 212° F there is an increasing
tendency for steam to escape. It is, there-
fore, desirable to reduce the steam flow
rate at this time, the so-called "trickle
finish." After the coldest corners have
reached 212°, the steam need be kept on
only enough to prevent the temperature
from dropping below 180° during the
next 30 minutes.
Preventing "blow-out"
Several additional precautions are
helpful in preventing "blow-out" and ex-
cessive steam loss.
The soil surface should be level, and
of uniform height above the steam out-
lets, so that steam will not reach the sur-
face at one point and escape, which
would decrease penetration elsewhere.
The soil should be well mixed and of
uniform moisture and compaction. Those
areas of beds which have been walked
on, or which are wetter than surrounding
soil, will heat more slowly than the rest.
Steam will, therefore, escape at the other
points before these are heated.
The introduction into soil of steam
under fairly high pressure may cause it
to form a channel to the surface. In such
cases, placing a pressure reducer in the
line will be helpful.
Depth and spacing of
steam outlets
The depth and spacing of steam out-
lets in a stationary mass of soil is im-
I L30 I
portant for the most efficient treatment.
They are determined in part by available
steam flow. The lower the flow rate, the
shallower should be the soil layer, and
the closer the spacing of pipes and the
holes in them.
In a unit with a single-layer steam
grid (Sec. 10, type 1) the pipes should
be so placed that the distance upward to
the soil surface is at least twice that to
the bottom of the container. In many
such units it is placed on the bottom. This
is in accordance with the tendency of
heat to rise. If the pipe is placed too close
to the surface, the steam will escape be-
fore most of the soil is heated.
In a unit with a multilayer steam grid
(Sec. 10, type 4) the distance between
layers should be 1% times that of the
depth of the top layer, and the distance
from the lowest pipes to the bottom of the
soil should be % the depth of the top
layer. This is because steam moves into
soil from the outlet in the shape of a
spheroid, enlongated at the top, as shown
in figure 71 and explained in Section 9.
When the zones of condensation in the
expanding spheres meet they do not over-
lap, and the steam probably then flows
toward the unheated corners. When all
soil is heated to 212° F, the steam will
diffuse out of the soil mass at every pos-
sible point.
The distance between steam outlets
able. The examples given in Section 9
will provide a basis for estimating proper
spacing of outlets for a given boiler
capacity.
Steam applied to soil surface
When steam is applied to the sur-
face of soil by either the Thomas or in-
verted-pan method (Sec. 10, types 18 and
19) the dependable depth of steam pene-
tration is about 8 inches. If this depth is
exceeded, steam escapes and does not
move efficiently through soil. This depth
is adequate for most benches. It may be
insufficient for ground beds to be used
for deep-rooted plants; in such cases it
is better to inject steam into the soil
through buried perforated pipes, buried
tiles, or moving rakes (Sec. 10, types 20,
22, and 23).
Steam applied to soil
in chambers
When pressureless steam is released
into a chamber surrounding soil in con-
tainers (Sec. 10, types 4b, 5, 6, 7, 8, 10,
11, 12, and 13), it is important that the
containers be separated by about %
inch in each direction. A method for
stacking flats is shown in figure 104
that permits unrestricted steam flow
without use of separator strips. Many
and between pipes should not be more nurseries prefer to place wooden sepa-
than 25 per cent greater than the depth
of the pipe (or of the top pipe in a
multilayer grid). The pipes may be
closer together than this, but they should
not be so close that the soil bridges on
them when it is dumped.
Decreasing the steam flow rate and in-
creasing the distance between steam out-
lets have the same retarding effect on
temperature rise in the soil mass (fig. 76
and Sec. 9). If a boiler of small output
volume is used, therefore, efficiency will
demand a closer spacing of pipes and
orifices in the soil mass than will be
necessary if a high-output boiler is avail-
rator strips between horizontal layers of
flats, and to leave a small crack between
vertical piles. All chamber steamers have
little escaping steam as long as there is
cold soil for it to condense on. As ex-
posed surfaces are heated, however, and
steam must penetrate farther through
soil before condensing, it escapes in-
creasingly from the chamber. For this
reason, it is inefficient to steam soil in
very large containers (such as tubs or
large planter boxes) by this method.
There is satisfactory efficiency in flats up
to 4 inches deep, since the steam then
only penetrates 2 inches through soil.
[131]
Efficiency will be improved by reducing
steam flow when excessive steam loss
from the chamber indicates that the con-
densation rate of the soil has been ex-
ceeded.
When steam is maintained under pres-
sure in a chamber (Sec. 10, type 9)
there is no problem of its escaping when
the condensing power of the soil is ex-
ceeded. Before beginning soil treatment,
the air must be fully displaced from the
autoclave by steam, in order to prevent
cold pockets. If this is carefully done it
will not entail excessive steam loss.
VOLUME OF STEAM REQUIRED
The quantity of steam produced by
the boiler and delivered to the soil
largely determines the quantity of soil
that can be heated, and the time required
to do it. It is, therefore, desirable to have
a boiler and steam mains of such ca-
pacity that the flow rate of steam does
not seriously limit the operation. The in-
formation supplied in table 14 and Sec-
tion 9 makes it possible to estimate the
size of boiler required for a given opera-
tion. The services of a heating engineer
will be helpful in calculating the capacity
of the boiler required for a specific situa-
tion, taking into account the efficiency of
equipment used.
If the operation is fairly simple, or if
the adequacy of an existing boiler is in
question, the capacity needed can be
roughly determined from the volume of
soil to be heated at one time. The follow-
ing examples give approximate calcula-
tions of steam requirements for various
types of operations. More exact methods
of calculation are presented later in this
section.
From table 14 in Section 9 it can be
calculated that approximately 6.5 pounds
of steam will be required per cubic foot
of a U. C.-type soil mix to raise the
temperature 150 degrees F in equipment
of about 50 per cent efficiency. Such ef-
ficienc) is attained or exceeded by equip-
ment in which steam is injected into the
stationary soil mass (sees. 9 and 10).
Examples are the Rudd type (type 1 ).
steam boxes (4a and 4b), buried per-
forated pipe (20), and buried tile (22).
The mobile bin (2) and combined bin
and potting bench (3) may attain such
efficiency if heat loss from the sides and
bottom is not excessive.
Thus, if a steam box containing 25
cubic feet of soil is to be heated from 62°
to 212° F, about 163 pounds of steam
(25 x 6.5 x ) will be required. A
150/
boiler delivering 200 pounds per hour
will be ample if long pipe and hose con-
nections are avoided, and if almost an
hour can be devoted to the heating. If
steaming needs to be done in a half
hour, a boiler delivering 400 pounds
might be required.
Similarly it can be calculated that ap-
proximately 10.8 pounds of steam will
be required per cubic foot of mix in
equipment of 30 per cent efficiency. Such
efficiency levels may be reached or ex-
ceeded with chamber-type equipment
when steam is released into space sur-
rounding containers of soil (sees. 9 and
10). Examples are the Thomas method
(types 5 and 18), vault (6), multipur-
pose tank (7), vertical cabinet (8), and
inverted pan (19).
Thus, if a bench of soil 3 x 10 feet x 8
inches deep is to be steamed by the
Thomas method, and the soil tempera-
ture must be raised 170 degrees F from
42°, about 245 pounds of steam will be
170\
required ( 3 x 10 x % x 10.8 x
1 50
boiler delivering 300 pounds of steam
would be adequate to treat the soil in an
[132]
hour, and 600 pounds would be needed
for a half-hour treatment.
Similarly, a pile of 100 flats, each
18 x 18 x 3 inches, heated 140 degrees F
from 72°, would require about 567
pounds of steam calculated as follows:
fiy2 x 1% x 14 x 100 x 10.8 x l^\ . A
boiler delivering 600 pounds would
heat these in an hour, and a 1,200-pound
unit in 30 minutes.
Among factors that the grower must
consider in selecting a boiler and treat-
ing equipment is the amount of soil that
must be steamed per day. Soil can be
treated in successive batches, but one
should be certain that enough batches
can be treated in a working day. If it
takes an hour to bring the soil to 212° F,
plus the required half-hour exposure,
and an hour to cool, unload, and reload
the unit, only 3 batches can be treated in
an 8-hour day. In designing the steam-
ing operation, the amount of soil per
load and per day is the proper starting
point in calculations.
PREPARING SOIL FOR STEAMING
Moisture content
The moisture content of soil to be
heated is very important in determining
the efficiency of the operation. It requires
about five times as much heat to raise
the temperature of a pound of water 1
degree F as it does a pound of soil (Sec.
9) . On the other hand, heat plus moisture
is much more effective in killing patho-
gens than is heat alone. Seeds start to
germinate if kept wet a few days prior to
treatment, and even the more resistant
weeds (Sec. 9) are then killed by treat-
ment.
These objectives are served if the soil
to be treated is moist enough for plant-
ing. After it is squeezed in the hand it
should crumble freely.
Dripping benches during steaming in-
dicate that the soil was initially too wet,
that the steam carried condensed water,
or perhaps that the flow rate was insuf-
ficient.
If the soil is very wet when steamed it
may come out in a soggy condition, be-
cause the water held increases the B.t.u.
requirement and more steam must be
used, which adds more water from con-
densation, in a vicious spiral. This will
be aggravated if the excess water does
not drain off readily, as in some ground
beds or heavy soil where evaporation is
not rapid.
It is always advisable to bleed the
water and moist steam from the pipe line
and hose near the point of connection to
the soil before treatment begins. If this is
not done, water is initiallv discharged
into the soil, causing increased B.t.u. re-
quirement, uneven soil heating, and wet
soil. For the same reason it is desirable
to use a water trap in the steam line near
the point of entry into the soil, so as to
continuously drain off the condensate.
This is particularly important if long
mains are used.
Freedom from lumps
U. C.-type mixes use fine sand of a
type which does not form hard clods
(Sec. 6). Even these, however, need to
be well mixed to avoid pockets of peat.
If lumpy soil is used, it should be pulver-
ized or screened before being steamed.
This is because clods are not readily
penetrated by steam I Sec. 9). Uneven
packing of the soil in the container also
makes for uneven heating.
[133]
UNEVEN HEATING
If soil heats unevenly during treat-
ment, one of the following factors may
be the cause.
Uneven compaction
Areas of beds which have been walked
or driven over will heat more slowly than
the rest, owing to reduced porosity of the
soil. The trouble is aggravated at high
rates of steam flow. The presence of
clods, just mentioned, also affects heat
penetration. Soil in benches or beds
should be well prepared and free of clods
to eliminate areas of compaction. In
boxes and bins one should not tamp the
soil, but let it settle firmly into place.
Uneven moisture
Soil with uneven moisture distribution
will heat unevenly, because of the greater
specific heat of water than soil. Soil
should never be watered after prepara-
tion and before steaming. Proper prepa-
ration will do much to make moisture
satisfactorily uniform.
Cold corners
"Cold corners" in boxes or bins have
been discussed above and diagrammed
in figure 71. The problem may be elimi-
nated by filling each corner with a tri-
angular wood block.
Excessive spacing of pipes
If pipes in a grid are too far apart,
relative to the steam flow rate, heating
will be so retarded that unevenness may
result, particularly if a clod or compact
or wet area occurs at the cool spot.
Uneven mixing
If the peat or other organic material
is not evenly mixed with the fine sand,
uneven heating may occur. Pockets of
dry peat are relatively impenetrable by
heat, owing to their insulating properties.
Insufficient steam
If the flow rate is insufficient for the
volume of soil treated, trouble with un-
even heat is aggravated. See "Efficient
Soil Steaming," above.
Partially frozen soil
Attempting to steam partially frozen
soil leads to uneven heating. It should
be thawed throughout, and mixed before
steaming.
Unexpelled air in autoclaves
Uneven heating in autoclaves results
when the air is not expelled before in-
creasing the pressure. The air should be
forced out of the exhaust valve or par-
tially open door by incoming steam for
several minutes, before closing the auto-
clave and beginning the treatment.
COOLING THE TREATED SOIL
Our experience is that flats may drop
to temperatures suitable for planting
within 1 or 2 hours, the time depending
upon exposure, air movement, and air
temperature.
The process of evaporation accelerates
the cooling of the soil. In uncovered beds
the temperature has been reported to
drop from 212' F to 160° in 1 minutes
at the surface, 2.6 hours at the 2-inch
level, and 8.3 hours at the 7-inch level. A
layer of canvas may extend the time of
cooling at the surface to 1 1 minutes.
Whenever treated soil is dumped and
piled on the floor, the surface should
previously have been wet down with a
formaldehyde solution (1 gal. to 18 gal.
water).
I K?41
WATER CONTENT AFTER STEAMING
Growers often ask whether steaming
does not make the soil excessively wet to
use. It may be calculated that, to raise the
temperature of 1 cubic foot of soil with
15 per cent moisture 150 degrees F,
would add 4.1 pounds of water, or 6.8
per cent, through condensation of steam
(assuming 80 per cent efficiency in heat
transfer). Senner (1934) showed that the
moisture in soil after steaming in-
creased by 2.3 to 8 per cent. Bunt (1954-
55) found an increase of 2.0 to 5.6 per
cent, and Morris (1954a) reported 5 to
7 per cent for light and 7 to 12 per cent
increase for heavy soil.
Actually much of this added moisture
is lost by evaporation as the soil cools.
Thus, in our tests with U. C. mix B (25
per cent peat) the final soil moisture was
increased by only 2.1, 3.6, and 3.9 per
cent after cooling. Even if evaporation is
reduced by stacking the flats or covering
the soil mass, the moisture content of a
U. C.-type mix has never been excessive
after treatment. For this reason we rec-
ommend that the soil to be steamed
should be moist enough to plant prior to
treatment.
There is no consistent difference in the
final moisture content of soil treated by
free-flowing and pressure steam, and this
is unchanged by rate of steam flow ex-
cept at very low, inefficient levels, where
it increases. Soil treated with super-
heated steam will be slightly drier (Sec.
9).
STEAM-TREATING HOME YARDS
The fact that soil may be treated in
proximity to plants suggests the pos-
sibility of the use of steam in home yards
against infestations of the oak-root
fungus, aster-wilt Fusarium, water molds,
and similar persistent soil fungi. A porta-
ble steam boiler and a steam rake with
pan (Sec. 10, type 21 1, could be used to
insure depth of penetration.
Such a practice would enable the
progressive nurseryman to cope with the
problem of existing infestation of soil in
home yards, so that the healthy plants
he sells will not be killed as previous
ones have been when planted there. This
investment in good will might also prove
to be profitable.
COST OF STEAMING SOIL
Because of the variation between nurseries in many operating conditions that
greatly influence the cost of soil steaming, no exact figure can be given for all situa-
tions. A hypothetical conservative example is given in detail so that the grower may
compare his own operations with it, and calculate his approximate cost.
Heat requirements
Assuming a soil with a specific heat of 0.2, 15 per cent moisture content, a weight
of 60 lb. per cu. ft., and the temperature to be raised 150 degrees F (for example
from 62° to 212° F), and water with a specific heat of 1.0:
B.t.u. for 1 cu. ft. soil = 60 lb x 0.2 specific heat x 150° F = 1.800
B.t.u. for water = 60 lb. x 0.15 moisture x 1.0 specific heat x 150° F = 1.350
B.t.u. requirement per cu. ft.
3.150
[135]
Assuming gas fuel of 1,100 B.t.u. per cu. ft. heat value and different levels of
efficiency in the total heat exchange: At 100 per cent efficiency, the gas used per cu.
3150
ft. of soil is _ ■,-■.. — z— - = 2.86 cu. ft.; at 70 per cent it is 4.09 cu. ft.; at 50 per
1100 x 1.00
cent it is 5.73 cu. ft.; at 30 per cent it is 9.55 cu. ft.
Cost of fuel
Using the most expensive (winter) gas rates (G-40 schedule), and assuming a
nursery of 60,000 flats per year, operating at 3 levels of efficiency in heat exchange:
60,000 flats == 1,000 cu. yd. = 27,000 cu. ft. of soil.
At 70 per cent efficiency:
27,000 cu. ft. soil x 4.09 — 110,430 cu. ft. gas required.
100,000 cu. ft. at $0,564 per thousand rate = $56.40
10,430 cu. ft. at $0,514 per thousand rate = 5.36
Cost for 27,000 cu. ft. soil = $61.76
Cost per cu. ft. soil =$ 0.002237
Similarly, at 50 per cent efficiency:
Cost per cu. ft. soil = $ 0.003130
Similarly, at 30 per cent efficiency :
Cost per cu. ft. soil = $ 0.005094
Cost per cu. yd. soil = $ 0.13754
Thus, with gas, the cost of fuel for steaming soil ranges from about 0.23 cent per
cubic foot at 70 per cent efficiency up to 0.51 cent at 30 per cent efficiency. Fuel oil,
costing about 0.078 cent per 1,000 B.t.u., as against about 0.055 cent for natural
gas, would make the cost about half again as much for fuel.
Cost of equipment
If a boiler is already used for heating glasshouses, this cost may be prorated and
will be less than the figures quoted below. These calculations are based on the pur-
chase of a small boiler, distribution lines, and soil-steaming equipment specifically
for this operation. A 25-day working month is assumed, with 3 batches of soil per
day.
27,000 cu. ft. per yr. = 2,250 cu. ft. per month
2,250 cu. ft.
— ^r— j = 90 cu. ft. per day
2d days
90 cu. ft.
TTi j — = 30 cu. ft. per batch, which must be heated in 1 hr.
o batches
This would require 324 lb. of steam per hr. at 30 per cent efficiency (30 cu. ft. x
10.8 lb. per cu. ft.; see "Volume of Steam Required").
Since efficiency has already been calculated, the boiler would need to be
324 lb.
— — — -, or 9.4 horsepower. A 10 to 15 horsepower boiler that would produce around
34.5 lb.
400 lb. steam per hr. would thus be adequate for this job.
[136]
Equipment cost of $3,000, with a 10-year life, and a 6 per cent interest rate is
assumed to provide the needed equipment:
... S3000
Principal, cost per year (depreciation) - = $300
10 yr.
Interest at 6 per cent, average per year = 99
Equipment cost per year = $399
$399
Cost of equipment per cu. ft. - = $ 0.014778
H ^ F 27,000
Total cost
Any additional labor introduced by the steaming operation is here omitted because
of the extreme variability in various nurseries. Furthermore, most of the handling
in a bedding-plant or gallon-can nursery will be necessary whether the soil is
steamed or not.
Cost of equipment per cu. ft = $0.014778
Cost of fuel (at 30 per cent efficiency) per cu. ft = $0.005094
Cost per cu. ft. of soil, exclusive of labor === $0.019872
It should be emphasized that these figures are very conservative, being based on
only 30 per cent heat efficiency, on gas at the winter rates, and include cost of the
boiler and equipment. The calculated cost of steaming is appreciably below that of
methyl bromide or chloropicrin fumigation (table 13), even when no equipment
cost is included for those treatments. Since the labor would be approximately the
same for each of the three methods, it may be disregarded. It is clear that soil steam-
ing is cheaper than fumigation, even when a boiler and equipment must be purchased.
The argument of the initial cost of the boiler, usually cited as the reason for fumigat-
ing rather than steaming, is shown to be economically unsound, even if money has
to be borrowed to purchase the equipment.
[137]
SECTION
Principles of Heat
Treatment of Soil
Kenneth F. Baker
Chester N. Roistacher
Temperature and time necessary for treatment
Objectives and definitions
Treatment of soil by heat
Treatment of soil by hot water
Treatment of soil by steam
HE IMPORTANCE of the soil in plant
culture has long been recognized by com-
mercial growers and botanists. It actually
supplies materials which make up about
85 per cent of the weight of green plants
( 80 per cent water, 2 per cent minerals,
and 3 per cent as hydrogen and oxygen
in carbohydrates), with only 15 per cent
taken from the air (carbon and oxygen
in carbohydrates). The justifiable early
practical interest in soils and in "root
action" quickly extended to include root
parasites after 1850-1880, once it had
been clearly established that plant dis-
eases could be caused by microorgan-
isms. Attempts were soon made to free
the soil of organisms injurious to plants
by treating it with heat or chemicals.
Heat sterilization had been demon-
strated to destroy fermentation organ-
isms as early as 1776, and to destroy
fungi in living plant tissue by 1883.
\bout L890, aspetic surgery, involving
heat sterilization of equipment, came to
the fore. About the same time (for exam-
ple, by B. Frank, 1888, in Germany)
steam treatment of soil was experi-
mentally used. W. N. Rudd (1893) in
Mt. Greenwood, Illinois, commercially
injected steam through perforated buried
pipes in the bottom of a bin of soil to kill
fungi, weeds, and insects, and similar
methods were soon adopted by other
growers. The Wutrick Brothers, Cleve-
land, Ohio, are said to have used the
steam-pan method about this same time.
It is to be noted that florists and nursery-
men were only a few years behind the
medical profession in the adoption of
steam sterilization. It has now become a
standard procedure in glasshouse opera-
tions the world over in order to reduce
losses from diseases, weeds, and insects.
This section presents the principles
and data supporting the practices out-
lined in Section 8 and the equipment
I 1^8 3
described in Section 10 for the heat
treatment of soil. This background in-
formation will provide a better basis for
present use of the suggestions outlined
in the preceding section, and is neces-
sary to the understanding of new de-
velopments. For example, the factual
basis for the use of steam-air mixtures
being developed in England is necessary
to understand and evaluate this method.
TEMPERATURE AND TIME NECESSARY FOR TREATMENT
Extensive studies by many workers in
various parts of the world have demon-
strated that exposure to moist heat at
150° F for 30 minutes will destroy the
important plant pathogens, insects, and
weeds (fig. 70) .
Fungi . . .
are relatively sensitive to heat. Rhizoc-
tonia may be eradicated from living
plant tissue by hot-water treatment at
125° F for 30 minutes (Sec. 13) ; the
most rigorous treatments recommended
have been 122° for 60 minutes. Water
molds are even more sensitive, Pythium
ultimum being killed in Aloe and Haw-
orthia plants at 115° in 20 to 40 minutes
(Sec. 13). The Botrytis gray mold is
killed at 131° for 15 minutes. The
gladiolus-yellows Fusarium is killed in
cormels at 135° for 30 minutes. The
cottony-rot Sclerotinia is destroyed at
122° for 5 minutes. Sclerotium rolfsii is
killed in 30 minutes at 122° in caladium
tubers and iris rhizomes (Sec. 13). Most
other pathogenic fungi are also destroyed
by time-temperature relations below
140° for 30 minutes.
Bacteria
Most bacteria that cause plant disease
are killed at 140° F for 10 minutes, and
probably all at 160°, since they do not
form the heat-resistant spores of some
animal pathogens and food-spoilage
forms. The data in figure 68 also show
that steaming at 212° for 30 minutes was
as effective as 8 hours in destroying the
spore-forming ammonifiers.
Nematodes . . .
are also quite susceptible to heat. The
root-knot nematode is killed at 118°
F in 10 minutes and is easily eradicated
in living plants (Sec. 13). The most
resistant foliar nematodes are killed at
120° for 15 minutes. The stem and bulb
nematode is killed at 127° for 11 min-
utes. The resistant, cyst-forming potato
root nematode, not known in California,
is killed at 118° for 15 minutes. The
lesion nematodes are killed at 120° for
10 minutes.
Insects and mites . . .
are also susceptible to heat, even in
the egg stage, and cannot long survive
140° to 160° F. Worms, slugs, centi-
pedes, and similar animals are ap-
parently destroyed by moist heat at 140°
for 30 minutes.
Weeds . . .
for the most part, are destroyed at
temperatures of 158° to 176° F for 15
minutes. In California nursery expe-
rience, however, three weeds survive tem-
peratures approaching 212°; these are
the button weeds (Malva), bur clover
{Medicago), and Lotus strigosus. In
other areas, shepherd's purse {Cap sell a ) .
Klamath weed (Hypericum), lambs
quarter (Chenopodium) , wild oat
(Avena), and some mustards are re-
ported to be quite heat-tolerant. Expe-
rience has indicated that seed of these
plants is not numerous in soils of the
type used in California. A fairly satis-
factory index of effectiveness of treat-
[139]
ment used by California nurserymen is
whether weeds other than the first three
mentioned appear after steaming.
Viruses . . .
of nursery plants do not persist in soil,
but some may survive in undecom-
posed plant refuse for a time. Thus, the
virus of chrysanthemum virus stunt will
live over in dried infected tissue for at
least 2 years, and will survive 200° F
for 10 minutes. In spite of this, soil
carryover of this virus is adequately
eliminated in commercial operations by
removal of most of the plant residue and
decay of the rest, and by steaming.
Tobacco mosaic, a similar virus with
respect to carryover, has been intensively
studied in the Department of Plant
Pathology glasshouses at the University
of California, Los Angeles, during the
past 7 years; the above procedures have
been so successful that there has been no
soil carryover, despite the fact that 212°
moist heat for 15 minutes is required to
destroy the virus in dead stems. The
majority of viruses are destroyed by tem-
peratures of about 160° for 30 minutes
and do not survive in the soil or refuse.
The use of a U. C.-type soil mix also
virtually precludes any virus carryover
because no host plants of troublesome
viruses occur in the source-areas of the
ingredients. Experience has shown that
growers following the U. C. system of
soil mixes and soil treatment have no
trouble with virus carryover.
Recommendations
Under ideal conditions, the organisms
of concern to growers may be killed by
heating to 140° F for 30 minutes, a fact
championed by A. G. Newhall at Cornell
University over the last two decades.
Since; commercial operations do not sup-
ply ideal conditions, a compromise with
reality is necessary. For example, clods
or lumps do not heat through as quickly
as loose soil, and there may be "cold
corners" in the equipment. To give a
working margin of safety we have, for
the past 16 years, recommended a mini-
mum temperature of 180° for 30 min-
utes. Before the development of the
U. C.-type mix, there was some danger
of soil post-steaming toxicity (Sec. 6),
and it was therefore desirable to keep
the temperature-time as low as possible.
Now that this is no longer a factor, even
higher temperatures are safe.
The present recommendation is to heat
a soil mix of the U. C. type to 212° F for
30 minutes, except that with equipment
in which uniform heating can be stopped
at 180° and held there for 30 minutes, it
is safe to do so. The temperature of 212°
is specified for steam because: (1) it is
often the only possible final temperature
for the process; (2) it is a temperature
that can be easily controlled (soil tem-
perature is not raised above that point
by steam, except under superheating or
pressure) ; (3) a U. C.-type mix develops
no post-steaming toxicity for plants and
may safely be heated to 212°; (4) the
extra cost of heating soil from 180° to
212° is less than 2.9 cents per cubic
yard1 and therefore economically not
important. With a U. C.-type mix it is
better to overcook than to risk incom-
plete heating. Other types of soils should,
when possible, be heated to only 180°,
until the grower finds that it is safe to
heat to 212°.
In continuous types of soil-steaming
equipment it is possible to control final
soil temperature to 180° F. In bulk types
of equipment it is practicallly impossible
to stop short of 212° if the soil is held in
the unit for the full time. If the soil is
dumped for "after-cooking", and is
mixed in the dumping, a uniform tem-
perature of 180° may develop.
' Based <»u L5 per cent soil moisture, 30 per
ccul Ileal olVwionry, and natural gas of 1,100
B.t.u. per cu. ft., costing $0,537 per 1,000 cu. ft.
[ 140]
OBJECTIVES AND DEFINITIONS
Heat treatment of soil is basically a
problem of transfer of heat from a
source, such as a boiler or heater, to the
soil particles. The objectives are to heat
the mass uniformly to 180° to 212° F,
to retain this temperature for 30 minutes,
and then to cool as rapidly as practicable.
Heat transmission through soils, like
biological phenomena of soils, is very
complex, difficult to resolve experi-
mentally, and therefore still imperfectly
understood. Background information on
the dynamics of heat flow through soil is
given to enable more efficient planning
and practical use of soil heat treatment.
As far as we are aware, this is the first
unified statement of the principles in-
volved in the various methods of heat
treatment of soil.
Heat is that form of energy resulting
from molecular motion, whose intensity
is measured by the temperature rise of
the receiving body, and quantity by the
B.t.u. (British thermal unit) received by
that body. The heat capacity of a sub-
stance is the quantity (calories) of heat
necessary to raise the temperature of 1
gram of it 1° C. This "heat storing"
capacity of water is very important in
the heat treatment of soils. Steam is the
vapor phase of water, which releases heat
as it recondenses to water. Heat and
steam move through soil in very different
ways, and must be clearly distinguished.
Because equipment used for soil treat-
ment employs either dry heaters or
steam, the movement of both heat and
steam through the soil is here considered.
(For steam, see p. 146 through 161. )
TREATMENT OF SOIL BY HEAT
Manner of Heat Distribution
The distribution of heat from a hot
to a cooler object is by conduction, con-
vection, and radiation. The importance
of each in soil is not fully clarified be-
cause of experimental difficulties. Con-
duction of heat is transmission through
a solid, liquid, or gas by those molecules
with greater energy transferring some of
it, without any mass motion, to their
neighbors of lower energy. The flow of
heat through a metal bar is an example.
Convection is the transfer of heat in a
liquid or gas by movement from the
hotter to the cooler area, as in the flow
of heat from a floor furnace. Radiation
is the transfer of heat through space
from one body to another not in contact
with it. Much of the heat from a fireplace
is of this type.
Conduction
Heat conduction through a porous
material is much less than through the
same material without pores, because
flow is greatly reduced by the contained
air, a poor conductor. On the other hand,
conduction is improved by the presence
of water in the spaces. Thus, dry sand-
stone conducts heat about 14 times
better than dry sand, about 7 times better
than water, and about 175 times better
than air, at temperatures with which we
are concerned. It follows that heat moves
by conduction through each soil particle,
and from soil particle to particle through
their numerous points of contact. It also
moves efficiently by conduction from
particle to particle across the water film,
and then has an enlarged area of contact.
Although water improves the contact be-
[141]
tween particles and so increases heat
transfer, if too much is added the heat
capacity of the soil is so increased that
there may be a decreased rate of tem-
perature rise. Patten (1909) reached
this point at about 18 per cent water con-
tent (dry-weight basis) for sand, about
10 per cent for fine sandy loam and silt
loam, and about 63 per cent for muck
soil (25 per cent organic matter). This
factor probably is not often important in
heat treatment of nursery soil, since
moisture is usually at lower levels.2
Conduction through actual contacts
and through water films is very im-
portant in heat transfer through soil.
Convection in the air spaces seems also
to be important, though less clearly
demonstrated. Generally considered to be
less significant are radiation from par-
ticle to particle through the pore air, con-
duction through the pore air, and con-
vection in the water film.
Thermal conductivity through various
types of mineral soil particles probably
varies little. Porosity, and therefore par-
ticle size and compaction is, however,
strongly related to transmission. Thus,
the percentage porosity in dry soil in-
creases, and the heat transmission de-
creases, in the following order: sand,
loam, clay, peat. Soil with particles of
several sizes tends to compact readily
owing to wedging of small pieces be-
tween large ones, which increases the
points of contact and therefore the con-
duction. Radiation across pores is also
2 In steaming soil, conduction is relatively
much less important, since heat is released by
condensation of steam directly on the soil par-
ticles (see "Treatment of Soil by Steam," be-
low). For this reason, in heating with steam
there is probably no improvement comparable
to that observed with dry heat, from the addi-
tion of water to the soil. At all but low mois-
ture levels, water actually tends to reduce
Bteaming efficiency by partially plugging the
pores and by increasing the total heat capacity.
This situation illustrates the necessity of clearly
distinguishing between steam and heat, already
mentioned.
increased, but convection is probably de-
creased.
Compaction generally improves move-
ment of heat. This, and several other
lines of evidence, indicate that conduc-
tion and radiation are more important
than convection in such movement. On
the other hand, compaction reduces
movement of steam and of chemical
fumigants by diffusion through the
pores. The addition of organic matter to
soil reduces heat transmission by in-
creasing porosity. Thus, Newhall (1940)
found that immersion heaters raised the
temperature of loam to 125.6° F in 3
hours and 147.2° in 4 hours, whereas
muck reached only 98.6° and 123.8° F,
respectively. Morris (19546) provided
a comparison between the rate of heat
transmission through soil by conduc-
tion, convection, and radiation, as
against steam flow. Insufficient heat pene-
trated through 1 inch of undisturbed soil
to raise its temperature to 160° F from
a steam grid resting on it, although dur-
ing the same period 15 inches of loose
soil above the pipe was raised above that
temperature. Steam flowed through the
soil above and released its heat, whereas
the temperature rise in the soil below
was probably largely from heat trans-
mission.
Another aspect of conduction in the
heating of soil is the distribution of heat
by the metal container or cooker. Steel
and iron are about 20 times better heat
conductors than moist soil, 150 times
better than dry soil, and 75 times better
than water. Consequently, the soil in con-
tact with the metal container will have
heat indirectly transmitted to it. Metal
liners are sometimes specified for treat-
ment equipment using immersion heat-
ers in order to take advantage of this dis-
tribution effect. Steaming of soil in gal-
lon cans involves very complex heat ex-
changes, since conduction by the can to
the soil, and steam flow into the soil sur-
face both occur.
[142]
Convection
Movement of heat through soil by con-
vection is directly related to pore size.
It is particularly effective in highly
porous soil, and probably is important
in heat transfer through a U. C.-type soil
mix. Bouyoucos (1913, 1915) has em-
phasized the importance of air convec-
tion currents in the transfer of heat
through soil. The magnitude of such
movement through the pore system is
shown by the normal exchange of soil
carbon dioxide and air with the atmos-
phere. It has been computed that the air
in some soils is completely renewed to a
depth of about 8 to 12 inches every hour,
and that this is largely by gas diffusion
through the pores ( Baver, 1956). The
rapid movement of methyl bromide and
other gases through soil pores during
treatment is further indirect evidence for
the importance of pores and convection
currents in heat transfer.
Although the percentage porosity of a
soil is inversely related to transmission
of heat by conduction and radiation, it
is misleading for estimating permeability
to gases. The number and size of the
large pores are of great importance here,
although much of the pore space is not
significantly involved in convection or
diffusion. Thus, coarse sand ( 37.9 per
cent porosity) is about 1,000 times more
permeable to air than is fine sand (55.5
per cent porosity) (Baver, 1956). Simi-
larly, a granular loam was 50 to 100
times more permeable than it was in the
powdered state.
Only a small amount of clay is neces-
sary in a sandy soil to reduce the pore
diameters and greatly reduce permea-
bility. Buehrer (1932) found that addi-
tion of 10 per cent clay to coarse sand
decreased air flow to about one fourth,
20 per cent clay to about one tenth, and
30 per cent clay to about one twentieth.
Clay soils may have 50 per cent porositv
and still be poorly aerated, whereas sand
with 30 per cent porosity may be well
aerated. He found that only part of the
spaces are involved in gas movement, a
considerable part of them being blind
alleys or so small as to greatly restrict
flow. Only in soil with coarse particles
does air flow reach levels to be expected
on the basis of percentage porosity. It
was concluded that only the larger and
continuous pore systems were significant
in air passage through soil. These would
be best provided by coarse or granular
soils with large bits of organic matter.
It would appear that conduction of
heat would decrease in the order sand,
loam, clay, peat, but that convection and
diffusion would be greater in peat and
sand than in clay and loam. When added
to a soil, water has the effect of reducing
pore size and permeability to air, de-
creasing convection and increasing con-
duction. This may contribute to the slow
heating of very wet soil by steam.
Gases increase in viscosity as the tem-
perature rises. Thus, the time in minutes
to pull equal amounts of air through
soil columns of moist sand, sandv loam,
clay, and peat, respectively, was found
by Bouyoucos (1915) to be as follows:
50° F = 1.50, 2.00, 15.00, and 16.40;
86° = 2.12, 3.37, 26.00. and 20.40;
122° = 2.50, 10.35, 33.00, and 38.40.
The viscosity of steam likewise in-
creases from 125.5 at 212° to 144.5 at
302° (54 lb. pressure), but since it
moves through soil at 212° F or less, this
is not a factor. This may contribute to
the greater efficiency of heat distribution
through soil by steam than by dry hot
air. Air convection would decrease as
the soil became hotter, and thus decrease
the effectiveness of the dry type of heat
transfer. Since the rate of heat inter-
change between a gas and porous object
through which it flows is proportional
to the temperature difference between
them, this also causes the rate of tem-
perature increase to fall off as the soil
gets hotter. On the other hand, water
convection would increase with rising
[143]
temperature, and thus aid heat transfer
in moist soils.
Radiation
Radiation of heat from the surface of
a soil particle occurs in a straight line
across the air space to another particle.
It is probably not very important in heat
transmission in soil, but has not been
evaluated. The efficiency decreases as the
pore size increases, and varies with the
nature of the exposed particle surface.
The radiation from the surface of the
particle is improved if it is moist, but
does not attain the efficiency of water
itself. It also improves with increasing
temperature.
Tests with soils
As the previous discussion has in-
dicated, the three methods of heat trans-
fer are not always affected in the same
direction by a given soil condition.
The conduction of heat by soil im-
proves as the percentage porosity and
pore size decrease, and as water content
increases. Convection is favored by many
large pores, but decreases in wet soil and
with increasing temperature. Radiation
is favored by small pores, wet soil, and
increasing temperature. It is thus ap-
parent that only by trial can the actual
heat transmission of a given soil be de-
termined. The results of such tests may
be instructive.
Von Schwarz (1879) placed soils of
61.7° F in contact with a heat source
(140°) and noted the temperature
reached in 15 minutes. Temperatures
reached by dry soils (increasing order
of transmission) were: peat 65.7°, clay
82.4°, loam 90.0°, sand 95.5°; for moist
soils these were: peat 69.6°, clay 102.6°,
loam 120.7°, sand 133.2°.
Bouyoucos (1913) measured the time
required for heat to pass from a source
(92.3° F) 7 inches through a column of
soil and cause the temperature to start
rising. For air-dry soil the figures (in-
creasing order of transmission) were:
peat 55.2, loam 49.7, clay 44.2, and sand
38.0 minutes. Similar tests with soils in
the field gave the following times (in-
creasing order of transmission) at 6
inches from the heat source: peat (148.6
per cent water) 9 hours, loam (36.6 per
cent water) 6.5 hours, clay (25.9 per
cent water) 6 hours, sand (3.6 per cent
water) 4 hours. In another test the time
at which temperature began to rise at
different distances in similar cores of dry
quartz sand and of moist loam, respec-
tively, were: 1 inch, 2 and 1 minutes; 3
inches, 15 and 16; 4 inches, 27 and 26; 5
inches, 34 and 35; 7 inches, 40 and 44.
From these and other data it would
appear that transmission of heat through
dry soil is best for sand, poorest for peat,
and intermediate for clay and loam soils.
Transmission of heat is improved in all
of these soils by the addition of water,
but the general order of transmission is
unchanged. It is probable, therefore, that
most of the transmission of heat is by
conduction, but that convection is also
important.
Rate of Heat Distribution
Dry soil
The rate of distribution of heat
through dry soil is as important as the
manner of transmission just discussed.
When dry soil is exposed at some point
to a constant heat source such as an im-
mersion heater, the temperature of the
soil directly exposed to the heat rises
fairly quickly. At a distance of 2 inches,
the temperature will begin to rise some-
what later, will rise more slowly, and
does not rise as high as at the source. At
4 inches it will rise later, slower, and to
a lower maximum than at 2 inches, and
so on. At any given distance there is
more heat flowing into the soil on the
"hot" side than is flowing out from the
cool side. This differential results from
the insulating effect of the dry soil, the
heat absorbed in warming the given
spot, and from lateral transmission of
I 144]
heat to surrounding particles or to the
atmosphere. The lateral flow is im-
portant because, as the sphere of heat en-
larges, the B.t.u. are being diluted into
an ever greater volume of soil (see
"Movement of Steam through Soil," be-
low) .
Wet soil
When the soil is wet, the advance of
heat is much the same, except that water
is evaporated near the source of heat and
condenses on the cool son" farther out.
This evaporation somewhat lowers the
temperature near the heater, and in ad-
dition the dry soil thus produced con-
ducts heat less efficiently than when wet.
Since the heat capacity of wet soil is
higher than dry, the temperature should
rise more slowly. These factors tend to
make the temperature of wet soil rise
more slowly than dry, at any given time
or distance near the heater. They are
offset, however, by the excellent heat
transfer by the steam formed, and by the
improved heat conduction of the soil at
a distance, so that the total effect of
limited additional moisture may be to
slightly increase the rate of heating. For
example, we found that an electric heater
that produced 120 B.t.u. per hour from
P/i inches of the tip exposed to a dry
sandy loam (0.88 per cent water) re-
quired 45 minutes to raise the tempera-
ture 32 degrees F at a 2-inch distance.
The same soil moistened to 7.11 per cent
water required only 39 minutes for this
temperature increase. Correcting for the
heat capacity of the water, the times
would be 43.1 and 28.8 minutes, respec-
tively. This again illustrates that conduc-
tion is the principal means of heat trans-
mission in soil. When heat is applied to
moist soil and the water at a given point
has been evaporated, the temperature
rise follows that described for dry soil.
Thus, heat applied to a moist soil is
intermediate between dry heat and steam,
more nearly approximating the former.
The steady and the
unsteady states
The above conditions apply when heat
is advancing through dry or wet soil —
the so-called unsteady state. If the heat
has been constantly applied for a suf-
ficiently long time, and the surrounding
conditions are also constant, each point
in the soil remains at a given tempera-
ture— the so-called steady state (fig. 72) .
At that time the temperature decreases
uniformly with distance from the source.
Temperature
Steady state
Distance from heat source
Fig. 72. Temperature gradients with distance from a heat source, in the advancing (unsteady)
and steady states. (Based on Patten, 1909.)
[145]
For a given heat input and surrounding
conditions affecting temperature loss,
there is a distance beyond which there is
insufficient heat transmitted for the soil
to reach 180° or 212° F. In practical
heat treatment of soil the steady state is
almost never reached, and the heat dis-
tribution through the soil is improved
by increasing the number of heat sources
per volume of soil.
One of the worst disadvantages of a
dry source of heat in soil treatment is
that intensity (temperature) is high,
quantity (B.t.u.) is small, and distribu-
tion is poor. Steam, by contrast, imparts
a large quantity of heat at low intensity
(212° F) and flows through the soil to
the cold areas. One of the principal ad-
vantages of steam is that the B.t.u. are
released at the point to be heated.
TREATMENT OF SOIL BY HOT WATER
Heat distribution by hot water in-
volves different factors than those out-
lined above. The water is applied to the
surface and flows by gravity through the
soil pores, heat being transferred to the
soil particles by conduction. The first
water displaces the air and fills the pores,
additional hot water pushes the cooled
water downward. The temperature de-
creases from top to bottom, and the low-
est level approximates the temperature
of the draining water. There is some
lateral spread, but not enough to heat
very far. Because even boiling water has
only 212 B.t.u. per pound, minus the
existing soil temperature, the tempera-
ture rise is very slow and a great deal of
water is required. Only 142 B.t.u. are re-
leased, for example, in cooling 1 pound
of water from 212° to 70° F, whereas
1,112 B.t.u. are released in similarly
cooling 1 pound of steam. Thus, with
soil at 70°, 7.8 times more moisture
must be added with boiling water than
with steam.
Because of the effectiveness of hot
water in leaching salts from soil, flood-
ing the propagating bench with it before
use is an excellent practice. If the messi-
ness of flooding with sufficient water to
raise the temperature to 180° F makes
heating in this way impracticable, the
leaching may well be followed with a
steam treatment to free the soil of patho-
gens.
TREATMENT OF SOIL BY STEAM
Condensation of Steam
in Soil
As the steam moves into the pores of a
soil it mingles with the air held there,
the ratio of steam to air rising with in-
creased time. The condensation of such
water vapor is determined by the tem-
perature difn rential between the vapor
and the soil particles, and by the ratio
of steam to air. as pointed out by Hoare
(1953), Morris (1954a), and Bunt
(1955).
The dew point is the highest tempera-
ture at which the quantity of water vapor
in the air is sufficient to saturate it and
cause condensation. The lower the con-
centration of water vapor (relative hu-
midity), the lower the temperature at
which condensation occurs. For ex-
ample, at 70° F all water vapor in excess
of 1 pound to each 63.3 pounds of dry
air will condense (fig. 73); at 100° the
critical ratio is 1:23.2; at 130°, 1:9.0;
at 190°, 1:0.9; at 211°, 1:0.03; and at
| I 10
Lbs. dry air
Fig. 73. Maximum pounds of dry air per pound of water vapor at which condensation occurs
at various temperatures. The ratio of steam to air at a given temperature may be determined
by reading down from the intersection of the temperature and the condensation lines. Thus, the
ratio for 90°F is 1:32. (Calculated from data of Zimmerman and Lavine, 1945.)
212°, 1:0 (that is, pure steam). This is
true whether it refers to condensation of
humidity in the glasshouse or of steam
in a bench of soil. These facts strongly
affect the manner in which steam heats
soil.
Relation of steam/air
ratio to condensation
When steam is released into soil of 70°
F, it expands if it has been under pres-
sure in the pipe, and drops to approxi-
mately atmospheric pressure and soon
to 212°. It condenses quickly on the
cool particles at its point of entry be-
cause of the low steam/air ratio (1 :63.3 l
at that temperature. As the temperature
of the soil and soil air rises from the
heat released by condensation, an ever
richer mixture of steam and air must be
reached if condensation is to continue
(for example, at 90°, this is 1:32.1).
On a given soil particle steam would con-
tinue to condense until the temperature
became too high for the existing steam/
air ratio. Since, however, steam is con-
tinuously released, and some air is
pushed ahead of the incoming steam, the
ratio rises steadilv until all air is dis-
placed. Condensation is, therefore, con-
tinuous until 212° is reached. The steam
then flows on to the cooler advancing
zone.
Incidentally, this principle explains
why an autoclave type of soil cooker op-
erating at 15 pounds' pressure must have
air displaced by steam (through operat-
ing with the exhaust or door open for a
time) before the temperature can reach
the expected 249.8° F.
[147]
Treating soil with
steam-air mixtures
From the above discussion on steam:
air ratio it is apparent that the steam
temperature may be reduced by injecting
and mixing air into the line near the out-
put. Recent investigations by Morris
(1954a) and Bunt (1955) in England
have ultilized this principle to heat soil
with steam to a final temperature below
212° F. By employing a venturi tube in
a steam line carrying 40 to 50 pounds'
pressure, enough air has been drawn in
to reduce the steam temperature to 160°.
If low-pressure steam is used, however,
a pump is necessary to inject air into the
flowing steam. When 180° steam is in-
jected into soil, the steam condenses on
the particles as before. The heated air is
pushed ahead, forming a band 3 to 4
inches wide, the temperature of which
remains between that of the heated and
unheated soil for 2 to 4 minutes. The
zone of condensation of 212° steam in
soil may be 1 inch wide or less (see be-
low) and remain for only 10 to 20
seconds. Savings of up to 15 per cent in
fuel have been reported. As already men-
tioned in this section, the calculated sav-
ing from heating soil to 180° instead of
212° is less than 2.9 cents per cubic
yard.
The method is not yet ready for com-
mercial application. When it is available
it can be attached to equipment types 1
to 8, 18 to 23, and 26 to 28 (Sec. 10).
Its application to equipment with a mov-
ing soil mass, or to pressure chambers, is
more doubtful.
Treating soil with a steam-air-
chemical mixture
The combination of a volatile fungi-
ride with a low temperature steam-air
mixture instead of with 212° F steam
(Sec. 10, type 26) would appear to offer
possibilities for effective cheap treat-
ment of soil. Since the velocity of chemi-
cal reactions increases two to three fold
CAUTION:
Many
of
the chemicals
mentioned
in this
manual are
poi-
sonous and
may
be
harmful.
The
user should
carefu
lly
Follow the
pre-
cautions on
the 1
abe
Is of the
con-
tainers.
with each 18 degrees F rise in tempera-
ture, it is evident why the combination of
heat and chemicals is substantially
cheaper than steam alone. Beachley
(1937) found that the combination of
formaldehyde with 212° steam reduced
by one third the time necessary for in-
verted pan treatment with steam, and
the cost by one fifth; it was one third
cheaper than a formaldehyde drench.
Soil conditions affecting
steam penetration
The air in the labyrinth of pores is ex-
pelled at a rate proportional to the
volume of steam injected; the rates are
not equal because of the volume reduc-
tion from condensation of the steam.
When large volumes of steam are used,
the air is displaced so rapidly by the
mass flow that it may not be appreciably
heated. With the usual smaller steam
quantity, the air is also heated as it is
pushed ahead, and transfers its heat in
turn to cooler soil particles. Since the
heat capacity of air is about half that of
steam (see Appendix), the quantity of
heat transferred in this way by air is not
large. It may contribute, however, to the
gradual temperature rise at a given point
in soil heated by inefficiently small
volumes of steam (figs. 75 and 76) . Cer-
tainly this air movement would reinforce
convection and diffusion in the continu-
ous soil pores. When air is injected into
the steam (see above) the importance of
heat transmission by the air is relatively
greater than when steam is used alone.
As already indicated, much of the soil
pore space is not involved in movement
of gases, there being many pockets and
plugged or partially blocked channels.
[148]
The steam flows freely along the open
channels, condensing on the adjacent
particles. The heat thus released is trans-
mitted to the surrounding particles by
conduction, radiation, and convection
within the sealed pores (see "Treatment
of Soil by Heat — Manner of Heat Dis-
tribution," above).
A clod of soil may be surrounded and
by-passed by steam before it has been
heated to 212° F. In a soil consisting of
uniform lumps, the thickness of the layer
being heated at any moment depends on
the rate of heat supply and absorption.
If both the lumps and the steam volume
are large, the vapor will be lost through
the surface during much of the opera-
tion. The same might apply to soil con-
taining many large pieces of organic
matter, or having cracks either in it or
between it and the container. In such
cases the width of the zone of condensa-
tion is determined by the depth of soil
treated (see also "Soil structure," be-
low).
Steam penetration of dry soil may
tend to be slower than for moist soil,
owing to the greater tendency to com-
paction and smaller pores of the former,
as well as reduced conductivity from low
moisture content. Water apparently af-
fects the flow of gases through soil
largely by its effect on pore size and soil
structure.
As mentioned earlier, when soil is too
wet, the high heat capacity of water re-
tards heating. Because of this, by the
time the water is heated to 212° F, so
much steam will have condensed that the
water-holding capacity of the soil will be
exceeded and water will drain from the
bottom of the bench (Sec. 8). This may
produce a broad temperature gradient in
the lower soil levels.
Movement of Steam through Soil
Steam moves through the air spaces
of the soil in the same way as any other
gas (see "Manner of Heat Distribution
— Convection," above). This certainly
involves diffusion, and probably also
eddy currents, through the continuous
pore system of the soil. Several facts in-
dicate that steam does move through
soil in this manner. It moves very slowly
through compact soil (for example, into
clods and subsoil — see "Soil structure,"
below). It moves more rapidly through
a soil to which organic matter is added,
or which is lumpy. Thus, we found that
at 5.54 per cent moisture and with a
single steam input of 3.5 pounds per
hour, a sandy loam required 33 minutes
for the temperature to rise 142 degrees F
at a distance of 5 inches, whereas U. C.
mix C (50 per cent peat) required but
18.5 minutes. Within limits, the larger
and more numerous the pores, and the
more continuous the system they form,
the better the penetration of steam. The
pores, however, must restrict the flow
enough that steam does not "blow out"
through the surface before condensing.
When all of the soil has been heated to
212° the steam does not condense, but
seeps out of the exposed surface; this is
visible evidence of the ready flow of
steam through soil. Pressure flow is
probably not involved in such move-
ment, as steam has little or no more than
atmospheric pressure in the soil.
With a small flow of steam
The way in which steam moves
through soil, and the rate of temperature
rise produced by it, are both strongly
affected by the volume of steam used,
and the distance from the point of in-
jection (see below, and figs. 74 and 76) .
When a small flow of steam is used, the
mixture of steam and air in the soil pores
at a given point becomes progressively
richer with increasing time and with
proximity to the input, as already ex-
plained. The pores of the soil around the
input are soon filled with pure steam,
and the temperature reaches 212° F. At
the moment steam was injected into soil,
the temperature in one of our tests was
188.4° (a steam air ratio of 1:1) 2
[ 149]
Wide
o
E
o
d)
Q)
c
o
to
N
D)
«-»-
c
o
t/5
_c
c
TD
~o
£
c
o
Narrow
Efficiency
Low
High
Low
Steam Flow Rate
Ratio of Steam to Air
High
Low
Fig. 74. Diagram showing the relations of steam flow rate to the steam: air ratio, width of
zone of condensation in soil, and efficiency. See p. 152 through 154 for explanation.
inches away, at 2% inches it was 148.2°
(a ratio of 1:5), at 3% inches 105.4°
(1:20), at 4 inches 76.8° (1:50), and at
5 inches 71.5° (1 :60) . Ten minutes later
the same relations would still exist, but
at greater distances from the input. Ap-
proximately the same situation exists for
higher steam injection rates at points in
the soil distant from the input (fig. 76).
That the ratio of steam to air is the
principal factor involved in the wide
condensation zone at low steam flow
rates is shown by data of the type
graphed in figure 75. In these tests with
U. C. mix C (50 per cent peat) we meas-
ured the temperatures at several dis-
tances from the steam input, and im-
mediately collected a large soil sample
from around each thermocouple to de-
termine, by oven-drying, the condensed
steam they contained. The temperature
curve and the percentage of moisture
both decrease with distance from the
steam input. The faster temperature rise
than would be expected from the amount
of condensed steam may have been
partly due to experimental limitations.
The suggestion is strong, however, that
there was some conduction of heat in ad-
dition to t lu- steam flow. It is largely to
preserve efficiency, by reducing the dis-
tance of steam travel, that perforated
pipes and steam rakes are placed at in-
tervals in a stationary soil mass in most
types of equipment (see below and Sec.
10), or that soil is broken into small
volumes by being placed in flats or pots.
It is apparent from these facts that
there is a wide zone (several inches) of
condensing steam in the soil under con-
ditions of reduced steam flow, both close
to and distant from the input. The width
of this zone in a given soil at a certain
distance from the steam input narrows
as the steam flow rate is increased.
The importance of heat transfer by
conduction, convection, and radiation
after condensation, in the case of steam
with a small flow rate, is not known. It
would be expected, however, that they
would become more important as the in-
put flow reached very low levels. When a
point is reached at which the heat lost
from exposed soil surfaces balances that
introduced by the steam, no further tem-
perature rise will occur (the steady
state) .
Transmission through soil of the heat
released by a small flow of steam would
fall off rapidly with distance. This is be-
cause of the B.t.u. required to heat a
given point of soil, and because of
1 1 ™ ]
lateral transfer of heat to surrounding
cool particles. Because of the increasing
volume of the spheroid of steam (see
below) , the number of cool particles and
the number of the plugged pores not
penetrated by steam increases in each
successive layer. Thus, there is the
double effect of the increasing volume of
soil for condensing steam, and the de-
creasing rate of transmission of heat
with distance.
These two effects are well illustrated
by MacLean's (1930) data on the heat
penetration of green pine logs in a
steam autoclave. In his tests, heat but not
steam penetrated the timbers. The tem-
perature at a given depth from the sur-
face decreased as the log size increased,
although other conditions were uniform;
the increasing volume thus presented
corresponds to the expanding spheroid
of soil discussed below. The temperature
also decreased progressively toward the
center of each log, despite the fact that
the volume became progressively less.
Thus the temperature decreased whether
volume increased or decreased. This in-
dicates that the decreasing transfer of
heat with distance through a solid is
more important in causing the lowering
12 3 4 5
Distance (in.) from steam input
Fig. 75. Relation of soil temperature and percentage moisture (condensed steam) with increas-
ing distance from the steam input. U. C.-type soil mix C, moisture-free at beginning of test,
injected with steam of 0.6 to 1.1 lb. per hr. for 12 to 20 min., when data were taken. Average
of three series. The temperature of the soil (broken line) and the per cent moisture (solid line) it
contains rise together. Both also decrease with distance from the steam input. This is because
the amount of air in the steam increases with distance from the input.
[151]
temperatures than is the increase of
volume from the enlarging sphere of
heat penetration. From this considera-
tion, the rate of temperature rise in soil
from transmitted heat may be described
as decreasing rapidly with distance be-
cause of resistance to heat flow, and this
decrease is reinforced by the enlarging
volume of the spheroid.
There is a further tendency for steam
of small flow rate to contain more en-
trained water than that of high rates,
because of greater relative condensation
in the lines. Low input rates often tend
because of this to diminish the pore size
in the soil and to further restrict steam
movement, particularly when the perfo-
rated pipes are on the bottom of a tight
bin of soil with poor drainage.
With intermediate and
high flow rates
Morris (1954a, 19546) has carefully
studied the movement through soil of
steam at intermediate and high flow
rates. It moves rapidly through porous
or lumpy soil or when a large volume of
steam is used, and more slowly in uni-
formly fine soil or with lower steam
volume. There is a maximum rate at
which a given soil can condense steam.
Beyond this rate the condensation front
becomes wider as the steam rushes by
particles without condensing, the steam
"blows out" through the surface, and ef-
ficiency is very low. At a somewhat
lower range the steam condenses in a
narrow zone whose thickness decreases
with the steam quantity. Morris and
Winspear (1957) were able, by using a
quick-acting thermocouple recorder, to
demonstrate this advancing condensa-
tion zone in soil. In one test, a point 21/i>
inches above the steam source increased
from 38.7° F at 2.12 minutes to 212°
0.75 minute later, a point 7% inches
above the source increased from 38.3°
at 9.25 minutes to 212° 1 minute later,
and a poinl L'3 inches above increased
from 39.0° at 17.38 minutes to 212° 0.5
minute later. Thus, the 212° front moved
10% inches in 15.01 minutes, or about
0.7 inch per minute. The front passed
the three points in 0.5, 0.75, and 0.25
minute, respectively (an average of 0.5
minute), and from this the thickness of
the front was computed to be only 0.35
inch. They concluded that, for efficient
use of steam, the thickness of this zone
should be 1 inch or less, and that the
total surface area of the soil particles
in the zone must be sufficient to condense
the steam supplied. In this range the ef-
ficiency is high.
It is apparent from the above facts
that at very low steam flow rates the
zone of condensation in soil is broad,
there is much mixing of the soil air with
steam, and efficiency is low. As the flow
rate increases, the condensation zone
narrows, the amount of air mixed with
the steam lessens, and efficiency rises.
Finally a flow volume is reached at which
the condensation zone is at its narrowest,
there is very little mixing of air with the
steam, and efficiency is at its highest. An
opposing factor begins to operate at
about this point: as the maximum con-
densing power of the given soil is
reached, there is an increasing tendency
for steam to "blow out" of the soil sur-
face. Once the condensing power of the
soil is exceeded, the efficiency falls
rapidly, because the mass flow of steam
rushes by the particles without condens-
ing. In this situation there is insignificant
mixing of air with the steam, the air be-
ing pushed out ahead of the steam, and
the condensation front again widens.
Thus, as the steam flow rate increases
from very low to high the width of the
condensation zone passes from very wide
to narrow, and again to very wide, as
different factors come into play. This is
schematically shown in figure 74. Be-
cause of the multiplicity of factors in-
volved, it is not possible to define the
limits of each of these levels of steam
efficiency accurately. It is obvious, how-
ever, that there is a lower, as well as an
[152]
upper limit for efficient use of steam.
Best commercial practice is to use a
steam flow just below the rate that gives
surface "blow out."
Expanding spheroids of steam
Morris (19546) investigated the
proper spacing of steam outlets in soil.
"It is a safe rule .... that the sterilising
effect can reach to 1V2 times the depth
of the pipes .... and the steam should
be injected at not less than % of the total
depth .... The space between the hori-
zontal pipes should not exceed the depth
of the holes by more than 25% and the
spacing .... along the pipe should be
about equal to the hole depth."
From these specifications, the findings
of Bunt (1954-55), and our observa-
tions, it is concluded that steam moves
out from an orifice into soil as a sphe-
roid with an elongated top, the margins
laterally and downward being approxi-
mately half that of the upward limit.
This is in accordance with the tendency
of heat to rise. The lateral movement
may exceed the downward flow by as
much as one fourth. This is the status
during the advancing state. When two
expanding spheroids overlap, the steam
probably flows toward the unheated
corners, because of the pressure reduc-
tion there caused by condensation of the
steam, and the fact that all of the pore
space at the point of overlapping would
already be filled with steam. When the
soil mass including all of the corners
and spaces between spheroids is heated,
each injection point will have heated a
rectangular volume whose dimensions
will be in the approximate ratio: dis-
tance from outlet to soil surface (or
lower limit of next rectangle above, in a
multilayer pipe grid) = 1.0; distance
from outlet to bottom (or to upper limit
of next rectangle below) = 0.5; distance
to lateral sides (or to lateral limit of ad-
jacent rectangles) = 0.5 to 0.625. This
relation is shown diagrammatically in
figure 71.
The farther out the steam flows from
the orifice the greater is the volume of
soil into which it passes. The approxi-
mate volume of the spheroid when the
steam has advanced 1 inch horizontally
from the input is 6 cubic inches, at 2
inches it is 50, at 3 inches 170, at 4
inches 402, at 5 inches 785, and at 6
inches 1,357 cubic inches. Because of
this sharp increase in the volume of soil
into which the steam passes in its out-
ward flow, as well as the factors already
mentioned, the rate of extension of the
spheroid of steam rapidly falls off with
distance from the source. It would thus
take about 215 times as long to heat a
6-inch as it would a 1-inch spheroid of
soil.
Increasing the distance from a fixed
steam flow has the same retarding effect
on temperature rise as does decreasing
the rate of steam flow at a fixed distance
(fig. 76), and for the same reasons.
Thus, in our tests a U. C. soil mix C (50
per cent peat) with 5.54 per cent mois-
ture reached 212° F in 8 minutes at a
point 6 inches from the input of 6.7
pounds of steam per hour, but only 3
inches from the input of 2.18 pounds
per hour. Distance and steam volume are
to this extent mutually compensating.
Efficient Rates of Steam Flow
Steam may be efficiently used over a
considerable range of flow rates and
penetration distances into soil. Neither
the steam volume nor the lateral distance
should be so great that steam escapes
from the surface before the mass is
heated. At the other extreme, the steam
volume should not be so small, nor the
distance between outlets so great, that
the heat losses from the surface and
sides offset the input, and necessitate
extended steaming periods. In other
words, the condensation zones should be
neither too wide nor too narrow, ap-
proximating 1 inch or slightlv less.
Efficient steaming thus requires that the
[153]
°F
210"
200-
190-
180-
170-
160-
150-
140-
130-
120-
110-
100-
90-
80^
70
U. C. Mix 6.7 lbs. per hour
2 in.
3 in. A .
4 in.
5 in , .
6 in
1 1 1 1 1
U. C. Mix 1.45 lbs. per hour
'5 in.
/ 6 in.
0 10 20 30 40 50 60
Time (min.)
U. C. Mix 3.5 lbs. per hour
/
/
k
1 — i — i — i — i — i
U. C. Mix 0.93 lb. per hour
U.C Mix 2.18 lbs. per hour
/6
Sandy loam 3.5 lbs. per hour
0 10 20 30 40 50 60
Time (min.)
—1 1
0 10 20 30 40 50 60
Time (min.)
Fig. 76. Temperature gradients of U. C.-type soil mix C (5.54 per cent water content) at five
distances from the steam input and at five steam flow rates. A chart for one comparable series
with sandy loam illustrates the effect of organic matter on steam penetration. See p. 153 and
155 for explanation.
[154]
temperature rise at any point should be
rapid, once it has started (fig. 74).
In tests at Los Angeles, U. C. soil mix
C (50 per cent peat) with 5.54 per cent
moisture was injected at a single point
with varying quantities of steam. The
times for the temperature to start to rise
from 70° F, and to reach 212° there-
after, respectively, 5 inches from the in-
put were as follows:
6.7 pounds steam per hour, 3 and
4 minutes ;
3.5 pounds, 10.5 and 6.5 minutes;
2.18 pounds, 10.9 and 21.7 minutes;
1.45 pounds, 22.5 and 52.5 minutes.
At the indicated rates of flow for the
total time to heat each 5-inch spheroid,
the B.t.u. required would be 754, 962,
1,149, and 1,758, respectively. This
series shows an increasing efficiency with
increasing steam flow into the spheroid.
Probably heat was transmitted to the
surrounding soil by conduction, convec-
tion, and radiation, and this played an
increasing role as steam flow was de-
creased. Since the upper limit of the
condensing capacity of the soil was not
exceeded, there was no falling off at the
higher volumes.
Bunt (1954-55) also found, for soil
in bins, a decrease in the amount of
steam per cubic foot of soil, and in time,
to reach 212°, as the steam flow was in-
creased. When a given volume of soil
was treated in 34 minutes, 7.35 pounds
of steam per cubic foot was required;
when the flow was increased so that only
8 minutes were required. 5.40 pounds
was used. He attributed the inefficiency
at low flow rates to heat losses from the
soil surfaces.
In our test the lower limit of practical
efficiency probably was the 2.18 pounds
per hour flow per orifice. At the 1.45-
pound rate, the temperature rise was so
slow (52.5 min.) that heat transmission
by conduction, convection, and radiation
probably came into play. One of the
principal advantages of steam (the re-
lease of B.t.u. at the point to be heated)
was, therefore, diminished.
Bunt (1954-55) found, on the other
hand, that thermal efficiency was greater
with moderate rather than with large
steam flow rates for soil in ground beds.
This is because there is less opportunity
for heat loss from exposed surfaces than
there is in benches or bins.
Steam "blow-out"
The upper limit of steam flow rate for
a given soil is recognized by the ten-
dency to "blow out" from the surface
before most of the soil is heated to 212°
F. Obviously this rate should not be
exceeded for efficient operation. It would
appear, furthermore, that the flow rate
should not fall far below this level for
maximum efficiency. The time for the
temperature to rise to 212° F several
inches from the steam input is a useful
measure of this range. In other words,
the steam flow should utilize fully, but
not exceed, the condensation capacity of
the given soil. Since this "balanced
steaming" is determined by so many
factors, it is best found by trial for the
given soil and conditions.
The tendency for steam to "blow out"
before the soil is treated may be mini-
mized by: (1) reducing the rate of steam
flow; (2) reducing the steam pressure at
the point of injection into soil; (3) hav-
ing the soil surface level, and of uniform
height above the steam outlets, so that
steam will not reach the surface at one
point and escape, decreasing penetration
at other points; (4) having soil well
worked and of uniform moisture and
compaction. In any case, efficiency is in-
creased by reducing the steam floiv to a
low level when 212° F is reached and it
begins to escape, the so-called "trickle
finish."
Spacing of steam outlets
The temperature rise to 212° F at a
point removed from the steam input is
[155]
never instantaneous, though in a prac-
tical sense it may appear to be. Even in
a case reported by Morris and Winspear
(1957) in which the temperature rose
from 38.7° to 212° F in 0.5 minute, the
reading at 0.25 minute was 135.5°. The
time increases with increasing distance
or decreasing steam flow. In one of our
tests it required 1.0 minute to heat U. C.
mix C (50 per cent peat) to 212° at 2
inches from a source injecting 6.7
pounds of steam per hour, and 7.5 min-
utes at 6 inches; at 3.5 pounds of steam
1.5 minutes is required at 2 inches, and
43 minutes at 6 inches. Thus, the proper
spacing of perforated pipes in the soil is
determined in part by the available
steam flow. Up to a point, greater dis-
tance between steam inputs is possible
without lessened efficiency, if the steam
flow rate is increased. With a flow of
about 7 pounds per hour from each ori-
fice, the spacing might well be 12 inches
or a little more without loss of efficiency.
However, if the flow is as low as 2
pounds per hour, the spacing should not
exceed 6 inches for a comparable effi-
ciency and time (fig. 76).
The soil mass settles during steaming,
presumably from the increased weight
of the water and from expulsion of air.
The settling may be as much as 4 inches
in 20 inches of soil, and it commonly is
1 inch or slightly more. This compaction
affects steam distribution. In a steam-box
soil treater with a rigid pipe grid having
holes on the underside of the pipes (for
example, type 4, Sec. 10), this settling
of the soil leaves an open space along
the underside of the pipe after steam has
been applied for a time. Steam fills this
space and thus diffuses into the soil from
a line, rather than a series of points. The
outward flow of steam probably begins
from the several orifices and gradually
extends to become a linear source along
each pipe. This would minimize the im-
portance of exact spacing of the holes in
the pipes in such equipment. Phis situa-
tion is not likely to occur with buried
perforated pipes or tiles because they
would settle with the soil.
Characteristics and
Forms of Steam
Water is an extremely efficient medium
for the transfer of heat. It changes form
from ice to water at 32° F, and above
that point stores heat at the rate of 1
B.t.u. per pound per 1 degree F rise, up
to the boiling point (212°). Thus, boil-
ing water contains 180 B.t.u. available
for soil heating above the freezing point
(fig. 77). At 212° another change of
form occurs, from water to steam, and
for this 970 B.t.u. per pound are neces-
sary, with no temperature increase (fig.
77). As is well known, water may be
brought to the boiling point much more
quickly than it can be boiled away, due
to these heat requirements. Thus steam
transfers its heat (970 B.t.u) in addition
to that of the condensed water (180
B.t.u.), or about 6.4 times as much as
does boiling water. About 6.4 times as
many pounds of water must be used
as steam to bring soil temperature from
32° to 212°. This explains the principal
disadvantage of the hot-water treatment
of soil (see "Hot-Water Drench of
Propagating Sand," Sec. 10). The prin-
cipal heat transfer by water occurs when
it changes to steam, and vice versa.
The existence of an advancing front of
steam must be appreciated in taking tem-
perature readings during soil steaming.
(See "Movement of Steam through
Soil," above.) The temperature rises
rapidly at a given point under efficient
operating conditions, and cold spots are
likely to be untreated and at the original
temperature. Readings should be taken
at points of slowest heating, and the tim-
ing started when these have reached
180° to 212° F. If the soil is adequately
protected from heat loss, it may not be
necessary to keep the steam on after this
time. Thermometers and Tempil Pellets
for measuring temperature are described
in Section 8 and the Appendix.
156]
1300
1200-
1100-
1000-
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1107
800-
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300-
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100-
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Free-flowing
dry saturated
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400
500
212
TEMPERATURE (°F)
Fig. 77. Relative amount of heat (B.t.u.) released by hot water, free-flowing steam, steam
superheated to four different temperatures, and saturated steam at six pressures. The available
B.t.u. for soil heating are indicated in each case. (Based on data of Keenan and Keyes, 1936;
Morris, 1954 b, has a similar graph.)
[157]
Free-flowing or
pressureless steam
The conversion from water to steam is
accompanied by a 1600-fold increase in
volume. If this change occurs in a boiler,
the degree of pressure may be regulated
by controlling the rate of fuel supply or
of steam flow.
Free-flowing steam without pressure
or superheating may deliver 1,150.4
B.t.u. per pound to an object at 32° F
on which it condenses. Of this amount
180.07 B.t.u. represents the heat residual
in water at 212°, and 970.3 B.t.u. the
heat released when steam condenses to
water (fig. 77). When steam is injected
into soil at 212° the heat is not trans-
ferred from the water since the soil itself
is raised to 212°, heat flowing only from
a warm to a cooler object. Only 970
B.t.u. per pound are therefore available;
but when soil is heated to only 180°,
there are 1,002 B.t.u. available.
Steam delivered from the boiler
through pipes is commonly under pres-
sure in order to deliver it in adequate
amounts. At 15 pounds' boiler pressure
the temperature of steam is 249.8° F.
However, when such steam is released
into the soil, the pressure is immediately
lost and the temperature drops back at
once to about 240° and then to 212°.
As this steam condenses it will yield only
about 14 B.t.u. more per pound of dry
steam than at 212° (fig. 77). The extra
heat content from the pressure is briefly
converted to superheat, and tends to dry
the steam by evaporating the water drops
it contains. The end result is usually,
therefore, to supply slightly more and
drier steam to the soil. Its effect on the
organisms is the same as the free-flowing
type, since they are subject to no pres-
sure.
Steam under pressure
I he flow may be restrained so that
boiler pressure will be built up, with
some increase in the heat available for
soil steaming. Thus, at 80 pounds per
square inch boiler pressure, there are
1,006 B.t.u. available (fig. 77).
Steam under pressure is most com-
monly used in cannery retorts or auto-
claves operating at 15 pounds' pressure.
Although this is an effective type of
equipment, the gain in heat transfer does
not justify the cost of a steamtight sys-
tem. Only 14 B.t.u. more per pound of
dry steam are delivered in such auto-
claves than by free-flowing steam (fig.
77) . If the pressure is increased to more
than 15 pounds, the equipment becomes
excessively expensive and there may be
restrictions to its operation. Further-
more, there is no effective decrease in
time of treatment or gain in efficiency,
because the autoclave must be operated
with the exhaust valve or door open for
a time to free it of air pockets before
pressure is built up (see "Relation of
steam/air ratio to condensation," above) .
Superheated steam
Steam may be superheated by passing
it through the fire box to heat it, much
as a furnace heats air. Because the
specific heat of steam is about half that
of water, there is a gain of only about
47 B.t.u. for each 100 degrees of super-
heat (fig. 77). At 300° F the gain would
be only about 43 B.t.u. This 4.4 per cent
gain causes almost no noticeable de-
crease in time of treatment, but con-
siderably increases the cost of equipment.
Steam superheated to about 450° was
used for a time in one commercial soil-
treatment operation in southern Califor-
nia; this gave an increase of about 114
B.t.u. (about 11.8 per cent) available for
soil treatment per pound of steam over
the free-flowing type.
In general, however, superheating is
more effective than high pressure in in-
creasing the heat content of steam; at
400° F it is 3.8 per cent, and at 500°
8.3 per cent better. Superheated steam
contains no unvaporized water and,
therefore, does not make the soil quite
as wet as does steam under pressure.
I L58 I
This, however, is not a critical factor
with good nursery soils.
It is questionable whether there is
enough gain over free-flowing steam at
212° F from either steam under pressure
or superheated to justify the increased
cost; in the ranges shown in figure 77
the gain is only 1.4 to 14.1 per cent.
Volume of Steam Required
It is desirable to have a boiler and
steam pipes of sufficient capacity that
quantity of steam will not be seriously
limiting at any time in soil treatment.
This means that the higher the boiler
horsepower rating (steam-producing
capacity) the faster a given soil mass
can be heated, or the larger the mass
that can be heated in a given time. One
boiler horsepower is the capacity to con-
vert 34.5 pounds of water at 212° F per
hour into steam at 0-pound gauge; it
equals 33,475 B.t.u. per hour. It is now
customary to rate boilers in pounds of
steam generated per hour. Boiler ca-
pacity bears no relation to steam pres-
sure, and a satisfactory boiler may be
of the flash type, without pressure, pro-
vided the steam does not have to travel
a long distance through pipes. Since
there is little gain in heat transfer
from using steam under pressure or in
superheated condition (fig. 77), the best
way to obtain the necessary soil-heating
capacity is to use a boiler of adequate
size.
Steaming too much soil for the boiler
capacity is inefficient owing to heat
losses through radiation, transmission,
and convection, as is permitting exces-
sive steam loss because of too small a
load. A balance must be worked out for
each piece of equipment, between too
much and too little steam for the volume
of soil treated. The assistance of a heat-
ing engineer is helpful in calculating the
required boiler capacity for a given soil-
steaming operation. However, a grower
can, to a large extent, adjust to the
capacity of a given boiler by:
1. Decreasing the area (in benches) or
volume (in bulk steaming equipment) of
soil treated, if it requires more than 1
hour to raise the temperature to 212° F.
«
Table 14. The Time Required to Bring a U. C.-Type Soil Mix to 212° F,
and the Amount of Soil That Can Be So Heated in 1 Hour
For 7 different boiler capacities and 3 levels of efficiency in heat exchange*
Boiler capacity
Equivalent
kilowatt-
hours t
Time per cu. yd. to
raise temperature to
212° F at 3 efficiency
levels; in min.
Maximum soil heated in 1 hr.
at 3 efficiency levels; in cu. yd.
Lb. steam
per hr.
Calculated
boiler
horse-
power t
30%
50%
70%
30%
50%
70%
100
2.9
28.4
175
105
75
0.34
0.57
0.80
200
5.8
56.9
88
53
38
0.68
1.14
1.60
300
8.7
85.3
58
35
25
1.03
1.71
2.39
500
14.5
142.2
35
21
15
1.71
2.85
3.99
1,000
29.0
284.4
18
11
8
3.42
5.70
7.98
2,500
72.4
710.9
7
4
3
8.55
14.26
19.96
5,000
144.9
1,421.9
4
2
2
17.11
28.51
39.92
* Computed on basis of 15 per cent water content in soil, 150 degree F rise in temperature, and specific
heat of 0.2.
t Computed on basis of 33,475 B.t.u., or 34.5 lb. steam, per boiler horsepower at 100 per cent efficiency.
Because boilers are often rated on the basis of area of heating surface, without regard to efficiency, these
figures may bear little relation to commercial horsepower ratings.
t Calculated on basis of 3,411 B.t.u. per kilowatt-hour at 100 per cent efficiency.
[159]
2. Increasing the area or volume of
soil, increasing the number of steam out-
lets in the mass, or simply reducing the
steam flow with a valve, or the pressure
with a regulator, if steam is escaping in-
stead of condensing.
The efficiency of the operation de-
pends on the proper balancing of all of
the factors by the grower.
Table 14 gives data on the time re-
quired for soil steaming with boilers of
various sizes, and for heat-exchange sys-
tems of different levels of efficiency. It
also presents data on the amount of soil
that can be treated in each case. Cal-
culated for a soil mix of the U. C. type,
this gives a steam requirement of 10.8
pounds per cubic foot of soil at 30 per
cent efficiency, 6.5 pounds at 50 per cent,
and 4.6 pounds at 70 per cent efficiency
to heat 150 degrees F. Bunt (1954-55)
found the requirement to be 5.40 to 8.45
pounds per cubic foot (average 6.51) to
heat clay loam 158 degrees.
A soil mix of the U. C. type with 15
per cent moisture would require 70 B.t.u.
per cubic foot per degree rise in tem-
perature at 30 per cent efficiency, 42
B.t.u. at 50 per cent, 30 B.t.u. at 70 per
cent, and 21 B.t.u. at 100 per cent effi-
ciency. Morris (1954a) obtained figures
ranging from 24 B.t.u. per cubic foot
per degree for compact, dry, light soil
at 9 per cent moisture, up to 53 B.t.u.
for compacted heavy soil at 58 per cent
moisture.
A safe working figure for steam re-
quirement in heating soil would appear
to be 6.5 pounds per cubic foot, or 42
B.t.u. per cubic foot per degree F.
Proper Soil Condition for
Steaming
Moisture content
The moisture content of soil to be heat
treated is of great importance in three
different ways.
I. // requires about five times as many
B.t.u. to heat J pound of water as it
does 1 pound of soil. The specific
heat of a light sandy soil has been
reported by Morris (1954a) as
0.192 and a heavy clay soil as 0.202
(both oven-dried), in comparison
with approximately 1.0 for water.
A peat soil had about the same
value as the heavy clay soil. An
average of 0.2 is generally used for
soils. Thus, to raise 1 pound of an
average soil 1 degree F requires
about 0.2 B.t.u. A soil with 20 per
cent moisture requires about as
many B.t.u. to heat the water as it
does the soil, despite the fact that
the water accounts for only about
one sixth of the total weight. Ex-
cessively wet soil often requires
twice as long to reach 212° F as one
in good planting condition, and it
is therefore uneconomic to steam
soil while it is soggy.
2. Heat plus moisture is much more
effective in killing microorganisms
than is heat alone, and soil should,
therefore, not be excessively dry
when treated.
3. Heat conduction of soil improves
with increasing moisture content,
and treatment therefore becomes
slightly more efficient.
As a practical compromise between
these opposing conditions, the soil to be
steamed should have sufficient moisture
to be in good planting condition, that is,
after being squeezed in the hand it will
crumble easily. When such soil is
steamed it comes out in good condition
for planting, without wasteful heating of
excess water, and with satisfactory de-
struction of microorganisms.
Soil structure
The structure of soil is important in
heat treatment because it affects the pas-
sage of steam and the conduction of heat
(see "Manner of Heat Distribution,"
and "Movement of Steam through
Soil," above) .
A clod is compressed, has reduced
L60 |
pore size, and therefore presents special
problems. It may be surrounded as the
steam margin advances, since it reaches
212° F throughout its mass more slowly
than does the porous soil. The time re-
quired increases with the size and com-
pactness of the lump, since steam diffuses
inwardly, and air is expelled simulta-
neously through the reduced pores.
Morris (19546) found that a lump 3%
inches in diameter did not reach 160°
at the center while the surrounding soil
reached 212°; one 5% inches in diam-
eter took 50 minutes to reach 212° at the
center; one 7 inches in diameter took
more than 1 hour to reach 160° at the
center. If lumps are covered by at least
2 inches of porous soil, they may be
heated through from transferred heat
during the after-cooking. They should,
however, be broken up as much as pos-
sible or removed by screening, to reduce
the chances of imperfect heating and of
"blow-through" by steam. Hoare (1953)
considered that the heating of clods,
even by this slow diffusion of steam, was
rapid as compared with the rate of heat
transfer by conduction.
Because uneven packing of the soil in
the container also makes for uneven
heating, particularly at high rates of
steam flow, it should be avoided (see
"Movement of Steam through Soil,"
above).
Soil must be as free of clods as pos-
sible for fast, successful, and economical
steaming. A U. C.-type mix uses soil of
such texture that resistant clods are not
formed (Sec. 6), and the whole problem
is thus avoided. If lumpy soils must be
used, they should be pulverized or
screened before being steamed.
In heating dry soil the picture is quite
different; heat is transmitted from par-
ticle to particle, and the smaller the pore
space the better. However, this treatment
method is inefficient for other reasons,
and is now little used. In treatment of
moist soil with heat, part of the thermal
transfer is by steam, as explained under
"Treatment of Soil by Heat — Rate of
Heat Distribution," above. The greater
moisture capacity of clay than sandy soils
is more important in determining the
greater number of B.t.u. required to heat
them than is the porosity or weight per
cubic foot.
[161]
SECTION
Equipment for Heat
Treatment of Soil
Kenneth F. Baker
Chester N. Roistacher
Considerations in the choice of equipment
Stationary soil mass treated in batches
Stationary soil mass in benches or beds
Moving soil mass in continuous output
Moving soil mass treated in batches
Equipment for generating and distributing steam
Soil treatment in a mechanized nursery
ROM THE discussions in the two pre-
ceding sections it is evident that there
can be no one type of soil heat-treating
equipment that is best for all purposes.
There are almost as many different
special models of equipment as there are
growers treating soil.
The grower must decide whether to
use a continuous type with a moving soil
mass or a batch type with static soil
mass, whether soil is to be treated in
bulk or in the containers, whether the
unit is to be stationary or mobile,
whether steam or dry heaters are to be
used, and whether the fuel is to be
natural gas, butane, oil, propane, or
electricity. It is a matter of finding the
type best suited to the given operation.
To provide the facts on which such a
choice must rest, the principles have
been discussed, and specific equipment
involving them is now presented.
Growers often develop equipment them-
selves, and rediscover designs already
abandoned by others. All basic types
are therefore described, even though
some are not recommended. References
are given so that further details may be
obtained.
CONSIDERATIONS IN THE CHOICE OF EQUIPMENT
Stationary versus
moving soil mass
All of the types of equipment used by
growers may be grouped into two
classes, according to whether the soil
mass is stationary or moving. On the
basis of efficiency, dependability, low
cost, and minimum recontamination
hazard we consider that the best type is
that in which the soil is treated by flow-
ing steam in planting containers (flats,
pots, beds) or /'// stationary piles (steam
[162]
chambers, autoclaves, Thomas method).
It does not follow, however, that all
nurseries should use one of these types.
// the heat source is steam, types of
equipment with a stationary soil mass
will prove best in most cases. If the
source is a dry heater of some sort,
thermal transmission will be much more
efficient and better controlled, with either
moist or dry soil, if equipment using a
moving mass of soil is employed. Conse-
quently, equipment of this type is con-
sidered best when dry heaters and either
dry or moist soil are used.
As explained in Section 9, it is
presently impractical with stationary-
type equipment involving the use of
steam to heat a soil mass uniformly to
less than 212° F, although this can be ac-
complished with equipment having a
moving soil mass. If heat is applied to
dry soil, the temperatures may rise well
above this point. With equipment treat-
ing a moving soil mass it is possible to
terminate the process at any desired
temperature by varying the heat input
(through control of the steam, gas, oil,
or electricity) or the time of exposure
(through regulation of the speed with
which soil is moved).
Provision for after-cooking
Merely heating soil to 180° to 212° F
is not sufficient; it must be kept at that
temperature for 30 minutes. Equipment
for continuously treating a moving soil
mass rapidly heats a small quantity of
soil and then dumps it. Provision must
always be made to keep the soil tempera-
ture at 180° to 212° F for at least 30
minutes. This can be accomplished by
quickly stacking the filled flats and
covering with a clean heavy canvas, or
by similarly covering the pile of soil.
Batch equipment for treating a sta-
tionary soil mass usually provides for
this after-cooking, but separate arrange-
ments must be made for the continuous
output from moving-soil equipment.
Is a boiler already available?
In general, there are two types of
California nurseries with reference to the
use of steam. One group operates glass-
houses and has a large steam boiler for
heating the range, or plans to install one.
The other and more common type does
not have steam-generating equipment,
either because only lath houses and out-
door plantings are used, or because the
glasshouses are heated by vented gas
stoves or unit heaters. The first group
may use their existing facilities, but the
latter must either procure a boiler or use
the self-generating or dry-heater types of
equipment discussed in this section.
Permanent versus
mobile equipment
A question that frequently arises is
whether to place the soil treatment and
handling equipment in a permanent loca-
tion in a nursery, or to maintain a
mobile unit. There are many modifica-
tions of each equipment type in use, and
the decision must rest with the grower.
Experience has indicated, however, that
there is less trouble with the boiler,
mechanical parts, and recontamination
when the soil is taken to the equipment,
rather than vice versa. With present
conveyer systems an efficient mechanized
nursery can be built around a single
soil-treating installation (Sec. 17).
Separating various operations
It is better if the various operations in
soil preparation are physically separated
in some way, so as to minimize recon-
tamination. For example, several nur-
series have divided them as follows:
1. A soil yard where storage and mix-
ing take place. The flats or cans may be
filled there if treating is to be done in
the container, and a mobile bulk cooker
may also be filled there.
2. The treating should be done at
another location or preferably in a
building so as to minimize wind-blown
[163]
Table 15. Summary of Characteristics of Equipment
+ = yes; - = no; — + = both yes and no apply because of dual function;
Characteristics
Equipment types* with soil stationary, handled in '
latches
External steam source
Generates own steam
3
Pi
1
a
A
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A
O
S
2*
A
o
a
B
a
>x
a
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Soil treated in containers
- +
- +
-
-
- +
+
+
+
+
+
+
+
+
- +
Treats containers separately
+
+
+
-
+
+
+
+
+
+
+
+
+
+
Powered moving parts used
Steam efficiently used
+
+
+
+
+
+
+
+
+
+
+?
+
+
+
Equipment inexpensive
+
+
+
+
+
+
+
-
+
-
+
+
+
+
Steam put into or surrounding soilf
IS
IS
I
I
IS
S
S
S
S
S
s
s
S
S
Soil heated above 212° Ft
Easy to load and unload
-
+
+
+
+ -
+
+
-
-
-
+
-
-
-
Type of steam used§ . .
FPS
FPS
FPS
FPS
FPS
FPS
FPS
FPS
FPS
P
F
F
F
F
Minimized recontamination hazard
- +
- +
-
-
- +
+
+
+
+
+
+
+
+
- +
Portable unit^
-
+
+
- +
+
+
-
-
-
-
-
-
-
- +
Also used for hot-water treatment of stock
-
-
-
-
-
-
-
+
-
-
-
-
-
-
Fits into mechanization
-
+
+
+
+ -
+
+
-
-
+
+
-
-
-
Type of fuel or electricity used||
GP
GE
GP
GPCE
Danger of burns or shocks
-
-
-
-
-
-
-
-
-
+
-
-
-
-
Treat around posts easily
Effective deep treatment of soil
Useful in small or large operations**. . . .
SL
SL
SL
SL
S
SL
SL
S
S
L
S
S
S
S
L64 |
for Heat Treatment of Soil. See Text for Details
? = variable or uncertain; blank = does not apply.
Equipment type
*
Soil in benches or beds
Soil moving
Continuous type
Dry source of heat
Steam
Hot
water
Steam-
formal-
dehyde
Steam
Dry source of heat
Batch
type
bo
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FPS
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FPS
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FS
FPS
FPS
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-
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E
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PG
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SL
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L
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S
SL
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S
S
S
S
S
S
* Numbers refer to equipment types in text; asterisks indicate best types for California conditions.
t I = into; S = surrounding.
X May, of course, be heated above 2123 F if superheated steam is applied for a long enough period.
§ F = no pressure, free-flowing; P = pressure; S = superheated.
^ Unit may be portable, but cannot be used away from special electric wiring (for example, 14, 15, 16). If units are portable when pro-
vided with a mobile steam source, they are so classed here.
I! P = type of petroleum; E = electricity; G = gas; C = coal.
** S = small operations only; L = adaptable to large operations.
[165]
dust. Filling of treated flats or cans with
treated soil may be done at the same
place or in the planting shed.
3. Planting of the containers usually
is done in another room.
With this compartmentalization of the
process there is small chance of dust
from the soil yard blowing into treated
soil. Care should be exercised, however,
to see that adhering untreated soil is not
carried on the mobile cooker from phase
1 to 3. There should be a concrete or
wood floor for phases 2 and 3, and this
might well be hosed down every day.
When treated soil is dumped in bulk
piles on the floor, the surface should pre-
viously have been wet down with a
formaldehyde solution (1 gal. to 18 gal.
water) .
Adapting batch equipment
to continuous operation
It is possible to capitalize on the effi-
ciency inherent in equipment treating a
stationary mass of soil, and yet operate
on a continuous-batch system. This was
done by a large commercial unit in
southern California that operated with
the method of the steam box (type 4) .
Two steam boxes were operated in se-
quence, one being filled with soil while
the other was cooking. Since the soil was
dumped directly into flat-filling equip-
ment, an almost continuous flow of
treated filled flats was produced.
Something of the same sort might be
done with the mobile bins (type 2), one
mobile bin being taken after treatment
and dumped into the flat- or can-filling
equipment while the other was being
filled and steamed. Two vault units (type
6) could be similarly operated in se-
quence, and the work mechanized by
placing the containers on pallets han-
dled by fork-lift tractors. This would
keep the boiler and the crew almost con-
tinuously active if the equipment were
properly designed. The same could be
done with two autoclaves (type 9)
operating in sequence, but the initial cost
would be high.
The important point is that it is not
necessary to use equipment with a mov-
ing soil mass in order to achieve con-
tinuity of operation, with the attendant
benefits of mechanization (Sec. 17).
Use of superheated steam
There is slightly greater heat trans-
mission and decreased water content in
superheated than in free-flowing steam
(Sec. 9). While it is not commonly used
because of the greater cost of the boiler,
it can be used with many of the types of
equipment described here, without their
modification in any way. Superheated
steam may be used with equipment types
1 to 8, 18 to 23, and 26 to 28 described
below.
Summary of Equipment
A summarized statement of the char-
acteristics, advantages, and disadvantages
of the 35 types of equipment is given in
table 15. One should use this tabulation
to determine the types of equipment with
the necessary features for a given instal-
lation, then refer to the text for details.
STATIONARY SOIL MASS TREATED IN BATCHES
Other things being equal, the sta-
tionary types are cheaper, easier to main-
lain, do not require power to drive
moving parts, and are less likely to break
down at crucial times, than are those
will) a moving ^<>il mass. In general, they
are also more efficient in the use of steam
because it is less likely to escape from
inside a static soil mass (before it has
reached 212° F) than from a moving
mass intermittently exposed to air. Types
I I through 17 have a dry source of heat.
[166]
Pressureless Steam from External
Source Released into Soil
1. The Rudd type . . .
first used in Illinois in 1893, repre-
sents the simplest form of this equip-
ment. It has been redescribed by several
stations in England, Europe, and the
United States, often as a new develop-
ment. It consists essentially of a bin con-
structed of wood, cement, or brick, lo-
cated on the ground so that it can be
loaded and unloaded from either the top
or one side (fig. 78). It is preferably
covered with a hinged lid. The dimen-
sions vary considerably, but the soil
depth should not greatly exceed 12 in.
Pipes of 1-in. diameter are laid in open
channels in the floor about 9 in. apart,
and are drilled on the underside with
%-in. holes 9 in. apart. The channels
may be covered by boards with V2_m-
holes. Alternatively, the pipes may be
partly imbedded in the concrete floor,
with the holes at the top; the pipes must
then lead into a condensate header from
which the soil may be blown before use.
The floor should slope slightly toward
one corner for drainage of condensate.
Such a unit may be used with free-flow-
ing, pressure, or superheated steam,
operating in all cases without pressure
in the box. If used for soil in containers,
this becomes the vault type (type 6). In
Norway a box with a steam grid in the
bottom is pivoted at the ends so that the
box may be easily tipped and dumped
after steaming. This idea might be ex-
tended to the steam box (type 4a) with
benefit. Advantages: very efficient use
of steam, simple and inexpensive; de-
pendable; no moving parts; can be used
for steaming pots and flats; may be
loaded by machinery. Disadvantages:
soil must be shoveled out, greatly in-
creasing recontamination hazard and
labor cost. Does not fit well into a fully
mechanized schedule. Best use: treating
soil in containers; treating containers.
References: Rudd 1 1893) ;x Fosler
(1950); Bewley (1948, p. 13-15, fig.
11); Lawrence and Bunt (1955).
A modification of this is to use tiles
instead of pipe, and use a deeper mass
1 See Appendix for complete references, cited
here by author and date.
Fig. 78. The Rudd type of steamer for stationary bulk soil (type 1). Fig. 79. The fixed-front
steam box for stationary bulk soil (type 4a). See also fig. 81.
[167]
of soil. References: Ball (1942, p. 3) ;
Roll-Hansen (1949, p. 7-8).
*2. The mobile-bin type...
used by several California growers elimi-
nates the above disadvantages. The bin
in this case may be the body of a
dump truck or a two-wheeled cart (fig.
80) that can be coupled to a tractor. The
pipe grid is on the bottom of the body as
before (temporary mounting in dump
truck), and a tarpaulin is used for a
cover. May be filled with a skip loader,
or conveyer belt from the mixer, and
emptied after steaming by tipping up the
front end and removing or tilting the
back panel. May be used with free-flow-
ing, pressure, or superheated steam,
operating in all cases without pressure
in the bin. Two units may be used in a
continuous-batch operation. Advantages:
very efficient use of steam; simple and
* One of the types considered best for Cali-
fornia conditions.
dependable; flexibility — may be ma-
chine-filled in soil area, connected to
boiler elsewhere, and dumped into flat-
or pot-filling equipment, on floor, or in
bins where needed; recontamination risk
reduced; may also be used for pots and
flats, or soil in containers; fits well into
mechanization. Disadvantage: some re-
contamination hazard. Best use: treating
bulk soil for bin storage, or for use with
flat-filler; also for pot and can growing.
References: Anonymous (1952) ; Morris
(1953).
3. The combined bin and
potting bench . . .
is a four-wheeled table with the ends
and one side fixed, and one side re-
movable (fig. 132). It is similar to the
mobile bin (type 2). A perforated pipe
grid is placed on the smooth metal floor
of the bin, which is then filled with soil,
covered with a tarpaulin, brought by a
tractor to the boiler, and steamed. The
Fig. 80. A mobile bin (type 2) soil steamer, trailer variant, for stationary bulk soil. Dump trucks
are sometimes fitted with perforated steam grids to give larger units of this type. A small portable
steam generator is shown at the rear.
[168]
pipe grid may then be lifted out, the
vehicle pulled to the potting site, one
side removed, and the potting done
directly on the bench. The unit may be
used with free-flowing, pressure, or su-
perheated steam, operating in all cases
without pressure in the bin. Advantages :
efficient use of steam; simple and de-
pendable; labor saving. Disadvantages:
considerable recontamination hazard
because whole load is exposed to in-
festation from the potting operation
when soil is first used; extreme sanita-
tion necessary; fair integration with
other mechanization. The contamination
hazard could be minimized by construct-
ing on the wagon bed a tapered soil bin,
from the bottom of which the soil flows
through a variable gate onto the potting
table. A permanent perforated pipe
steam grid could be built in the bin. The
treated soil would be thus protected from
recontamination until used. Best use:
pot-plant growing. Reference: Anony-
mous (1954).
*4. The steam box . . .
is a wooden or metal box equipped
with a hinged lid for filling with soil,
and a dump bottom for emptying. It is
elevated from the floor, and is stationary
( or may be mounted on wheels for
mobility, if fabricated of metal). If it is
made of wood, resin-impregnated marine
plywood2 must be used, as others will
deteriorate when steamed. The "cold"
edges and bottom four corners should be
fitted with triangular pieces of wood to
expedite uniform heating. These four
corners are usually the coldest spots in
all batch treating equipment. In the box
is a perforated grid of pipes arranged in
rows 9 in. apart each way; on the under-
side Vs-in. holes are drilled about 9 in.
* One of the types considered best for Cali-
fornia conditions.
2 Phenolic resin glueline and coating on sur-
faces; may be called High Density Overlaid
Plywood.
apart. This arrangement insures that no
soil particle is more than 5 in. from
several steam outlets, which provides
maximum efficiency in distribution of
steam and speed of heating. It is filled
from above, emptied below. There are
several methods for operating the bottom
doors; among the best are controlled
lowering by a chain hoist, rack and
pinion gears, sprockets and chains, or by
a cable wound on a racheted shaft; a
mechanical trip-catch on free-falling
doors may also be used.
It may be made with a fixed front
(type 4a; figs. 79 and 81) for bulk soil
only, or with the front panel removable
(type 4b; figs. 5 and 82), so it may be
used for bulk soil or for flats and pots,
empty or filled with soil, these being
placed on the pipe shelves. The units
were developed by the authors in the
Department of Plant Pathology, Univer-
sity of California, Los Angeles. A Los
Angeles company will fabricate such
boxes on special order (see Appendix).
When used for flats, steam is released
into only the bottom layer of pipes, the
valve closing off the other pipes. The
bulk-soil type is useful for nurseries
with fairly large soil requirements, since
the box may be dumped once an hour,
or oftener if a large steam flow is used.
Continuous-batch operation may be
achieved by having two boxes in tandem,
one being filled while the other is steam-
ing. Such a unit was successfully used on
a contract basis in southern California
for several years, turning out about 16
cu. yd. per day. When such a dual unit
is coupled to an automatic flat-filler
(Sec. 17), an essentially continuous
output of flats is obtained. Anv of these
units may be used with free-flowing,
pressure, or superheated steam, operat-
ing in all cases without pressure in the
box. The front-opening tvpe is probablv
the best available for the small nursery,
because of its flexibility and efficiency.
These boxes are probably the most effi-
[109]
Fig. 81. The fixed-front steam box for sta-
tionary bulk soil (type 4a). See also fig. 79.
cient. dependable, and convenient of the
bulk-type equipment, and fit admirably
into mechanization. For example, a
Toledo, Ohio, nursery is said to use
boxes of this type holding 3% cu. yd.,
arranged so that the soil drops directly
into dump trucks. Advantages : very effi-
cient use of steam; rapid and uniform
heating of soil; simple and fairly inex-
pensive to construct; very dependable,
with few moving parts; highly adaptable
in the various forms, fitting well into
mechanization; cannot be overheated
(unless used with superheated steam) ;
ease of handling; containers also treated
(in open-front type only). Disadvan-
tages: since containers are not treated
(except in open-front type), this must
be done separately; some recontamina-
tion hazard with bulk type, as soil must
be handled. Best use: bulk-soil type,
single or dual, with or without attached
flat-filler, is excellent for large nurseries.
Open-fronl type nearly ideal for small
nursery. Reference: Roislacher and
Baker (1956).
I I
Fig. 82. The removable-front steam box for
stationary bulk soil, and for soil in containers
(type 4b). See also fig. 5.
PressureSess Steam from External
Source Released around Soil
*5. The Thomas method for
steaming soil in containers . • .
should be more widely used. The prin-
ciples and methods are the same as
described for the surface Thomas
method (type 13; see fig. 91). Flats or
pots are stacked on the concrete floor
with wood separators between layers, or
in special steel racks, and covered with
a rubberized canvas or similar material.
The tarp is held down by pipes or sand
bags along the edges. Steam is released
under the cover, which then acts as a
steam chamber. The method may be used
with free-flowing, pressure, or super-
heated steam, operating in all cases
without pressure in the soil. Advantages:
inexpensive, simple, efficient; materials
readily available; used for any con-
tainer, empty or full; also used for bulk
soil (type 18) ; adaptable to mechaniza-
* One of the types considered best for Cali-
fornia conditions.
70 |
tion by use of pallets and fork-lift trac-
tor. Disadvantages : cover may wear out,
particularly if paper; takes up work
area unless a separate floor is provided.
Best use: small nursery; larger opera-
tions should use permanent equipment.
Reference: Dimock and Post (1944).
*6. The vault type . . .
has been used for at least 25 years,
and is still one of the best for soil in
flats and pots. It consists of a vault built
of reinforced concrete, planks, or heavy
resin-impregnated marine plywood,3
with a concrete floor continuous with that
outside (figs. 83, 128, and 131 ) . A swing-
ing wooden door on one end is sealed
around the edges with a gasket of rubber
steam hose, and held tightly closed by
several refrigerator-type door clamps.
The unit is not steamtight and will not
build up pressure. The steam will con-
dense on the soil, with only slight leak-
age from the vault, until the inside
temperatures approach 212° F, when
increasing amounts will be lost. The
steam is admitted to the vault from a
perforated pipe on the floor against the
sides and back end, with the holes
toward the inside of the vault and down-
ward on a 45° angle with the floor. Such
a vault may be loaded manually, flats
being stacked with %-in. separator
strips or as shown in figure 104, and pots
set on top of each other. A better system,
however, is to pile the flats or pots on
pallets and load these into the vault with
a fork-lift tractor. While such a vault
can be used for bulk soil in large boxes,
it is less efficient than the perforated
pipe grid for this purpose. These units
may be built in any size, depending on
the needs of the nursery and on the
boiler capacity. Two vaults may readily
be used in a continuous-batch operation.
The equipment may be used with free-
flowing, pressure, or superheated steam,
operating in all cases without pressure
in the vault. Advantages: soil steamed
directly in containers, reducing both the
handling after treatment and the recon-
tamination hazard; quite efficient use of
steam; convenient; dependable, without
moving parts; quite inexpensive to
build; adaptable to any type of con-
tainer, empty or full, and even bulk soil
(with lowered efficiency) ; fits well into
a mechanization program; heating soil
above 212° F is possible only with
superheated steam. Disadvantages: may
be awkward to load and unload man-
ually, with some chance of getting
burned; if soil load is excessive for
boiler capacity, treatment may take
several hours; poorly adapted for treat-
ing bulk soil. Best use: excellent in
general growing operations, manually
handled and of small size in small nur-
series, mechanically handled and large
for bigger ones. Reference: Newhall,
Chupp, and Guterman (1940, p. 33-34).
*7. The multipurpose-tank type . . .
is a modification of the vault steamer
designed so that it may be used for soil
and container disinfestation, and also as
a hot-water tank for treatment of seeds,
bulbs, and planting stock (Sec. 13), as
well as a soaking and steaming tank for
pots, cans, and flats. This combination
was suggested by C. E. Scott, California
Agricultural Extension Service, and the
equipment designed in 1940 by H. Gor-
don, Department of Agricultural Engi-
neering, University of California, Davis.
It has been extensively used by the De-
partment of Plant Pathology, Los An-
geles, for 16 years and has proved to be
the "work horse" of our treating equip-
ment. It consists essentially of an in-
sulated horizontal metal shell, with a
hinged lid (figs. 84 and 85). The lid is
loosely sealed with a gasket of rubber
steam hose. Steam is released through a
perforated pipe in the bottom of the tank.
* One of the types considered best for Cali-
fornia conditions.
3 See footnote 2, above.
[171]
83
S-**c
^^S^^^^S^S^SSSk
^^S^r^S^S
84
Fig. 83. (Top) The vault-type steamer for soil in stationary containers (type 6). See also figs.
128 and 131. Fig. 84. The multipurpose tank (type 7) for steaming soil in stationary containers,
for hot-water treatment of planting material, and for soaking salt from pots. See also fig. 85.
I 172]
Fig. 85. The multipurpose tank (type 7) for steaming soil in stationary containers, for hot-water
treatment of seeds and planting material, and for soaking salt from pots. Note the outlet pipe for
circulating water in left photo, and pump and input in the view on the right. The input pipe is
fitted with a valve, and also serves as the drain pipe. A thermometer is placed in the input line.
The steam input pipe (white), and method of stacking flats are shown. See also fig. 84.
The unit is not steamtight and cannot
build up pressure. It may be operated
on free-flowing, pressure, or superheated
steam. Into this container may be
stacked soil in flats, cans, or pots, with
the layers separated by wood strips. It
may also be used to steam empty con-
tainers prior to use. The tank may be
filled with water and heated by passing
steam through a pipe in the bottom, with
the condensate passing out of the tank,
or steam may be released directly into
the water. The temperature may be ac-
curately controlled by adjusting the
steam valve. The circulating pump re-
moves the water from the top at one end
and returns it to the bottom at the other,
providing excellent water circulation.
Used in this way the unit has proved
very efficient for the hot-water treatment
of seeds, corms, and whole plants. With
or without the circulating pump oper-
ating, it provides an excellent tank for
soaking the salt out of pots (Sec. 4).
Such units can be built in a size suitable
for the given nursery. Advantages: soil
is steamed directly in the containers;
quite efficient use of steam (it should be
turned very low when condensation has
nearly ceased and much steam is escap-
ing) ; dependable, without moving parts;
quite inexpensive to build; adaptable to
any type of container, empty or full;
heating soil above 212° F is possible
only with superheated steam; extremely
flexible, triple-function unit. Disadvan-
tages: awkward to load and unload;
poorly adapted for treating bulk soil;
does not fit well into mechanization.
Best use: excellent for general growing
operations, particularly where heat
treatment of seeds and propagative ma-
terial is planned; best suited for triple
function in small nurseries and in experi-
ment stations.
8. The vertical-cabinet type . . .
consists of a wood (marine or resin-
impregnated plywood4) or metal cup-
board, on the shelves of which are placed
flats, pots, or cans of soil to be treated.
4 See footnote 2, above.
[173]
Steam is released into the bottom of the
cabinet and condenses on the cool con-
tents as outlined for the vault type (type
6). Apparently this was first adapted
from self-generating equipment used for
dairy utensils. The usual form is a wall
cabinet with pipe shelves on which flats
and pots may be placed. The door should
have a gasket of rubber steam hose.
Similar to the vertical-cabinet type (type
11; fig. 88). May be used with free-
flowing, pressure, or superheated steam,
operating in all cases without pressure
in the cabinet. Advantages : soil steamed
directly in the containers; quite efficient
use of steam; dependable, without mov-
ing parts; inexpensive; adaptable to
various containers, empty or full; heat-
ing soil above 212° F is possible only
with superheated steam; soil not han-
dled after treatment. Disadvantages : not
adapted to large volume or to bulk soil;
awkward to load and unload; does not
fit well into mechanization. Best use:
small nursery using flats, pots, or cans,
and not requiring bulk soil. Reference:
Johnson (1930, p. 4-5).
Pressure Steam from External
Source Released around Soil
9. Autoclaves or cannery retorts . . .
(figs. 6 and 86) are sometimes used for
soil treatment. Usually they are second-
hand, as cost would otherwise be pro-
hibitive. When used at 15 lb. steam pres-
sure, the exhaust valve or the door must
be left open for a time to displace the
air with steam. Sometimes operated as
pressureless containers, when the unit
becomes the vault type (type 6). Heat
transfer by steam at 15 lb. pressure is
only 14 B.t.u. per lb. greater than when
free-flowing, and the temperature only
37.8 F higher (fig. 77). May be mech-
anized l>\ stacking containers on pallets
thai are loaded into autoclave with a
lork-lifi tractor. Two autoclaves could
be used in tandem in a continuous-batch
operation. Advantages: slightly faster
heating (about 1.4 per cent) than with
flowing steam; soil treated in contain-
ers; efficient; dependable, without mov-
ing parts; fits well into mechanization
program; adaptable to any type of con-
tainer, full or empty. Disadvantages : re-
quires pressure boiler to operate it; high
initial cost; difficult to load and unload,
with some chance of getting burned; soil
heated to unnecessarily high tempera-
ture; if air is not displaced by steam be-
fore closing the door very uneven heat-
ing may result. Best use: general grow-
ing operations in medium to large
nursery. Reference: Newhall, Chupp, and
Guterman (1940, p. 33).
Pressureless Steam from Built-in
Generator Released around Soil
Several kinds of soil-treating equip-
ment may be modified in such a way
that water may be converted to steam
inside the unit by heat supplied from
gas, oil, butane, or propane flame, or by
electricity. Usually a metal pan of water
is heated until sufficient water is evapo-
rated to raise the temperature to 180°
to 212° F. To be effective, therefore,
such units must contain that amount of
water, plus an excess to avoid boiling
dry. To raise the soil temperature of 1
cu. ft. of soil with 15 per cent moisture
150 degrees F will require that about 6V2
lb. (about 61/4 pints) of water be con-
verted to steam, assuming 50 per cent
efficiency. Equipment of this sort usually
contains up to twice this amount of
water.
10. Horizontal type with
removable hood . . .
is used by several nurseries in Califor-
nia. It consists of a metal pan contain-
ing water underneath a rack on which
flats or pots are stacked. A large metal
hood is lowered over the stack by a hoist,
to form the steam chamber (fig. 87).
Heat is applied by gas or oil burners
[174]
86
g g *?*
Fig. 86. Cannery retort (autoclave) for steaming soil under pressure in stationary containers
(type 9). See also fig. 6. Fig. 87. Horizontal type of steamer with removable hood (type 10).
Steam is generated from the water in the metal pan below, and containers of soil are stacked
on a wooden frame above it. Fig. 88. The vertical cabinet type of steamer (type 11) for steam-
ing soil in stationary containers. Steam is generated from the water in the metal pan below.
Steam may be released into the cabinet (type 8); the metal pan is then omitted.
[175]
under the pan, or by electric immersion
heaters in it. If externally generated
steam is released into such a unit, it es-
sentially becomes a vertical-cabinet type
(type 8). Two such units could be used
in a continuous-batch operation. Ad-
vantages: soil treated in containers; in-
expensive; cannot be overheated; fairly
efficient use of steam; easy to load and
unload; fits fairly well into small-scale
mechanization. Disadvantages: not use-
ful for bulk soil; slow operation; im-
practical for more than 16 flats per load.
Best use: small nursery having little
need for bulk soil; home garden or
hobby greenhouse. Reference: Califor-
nia Dept. Agr. (1944).
1 1. Vertical-cabinet type . . •
is a modification of type 8 above, in
which a metal pan in the bottom holds
water which is heated by a gas burner
or electric elements (fig. 88). Uses 1.2
to 2.0 k.w.h. per cu. ft. of soil. In Eng-
land the "saucepan" and "trough" meth-
ods are small-volume variants of this
type. None of these types fits into a
mechanization program. References:
Peterson (1942) ; Newhall (1940, p. 19-
25) ; Lawrence and Newell (1950, p. 83-
84) ; Lawrence (1956, p. 47-49).
12. Modified-oil-drum type . . .
is sometimes used by very small nurs-
eries in California. An oil drum is
mounted vertically on a brick base so
that gas or oil burners may be placed
under it. Inside there is fitted a metal
base to keep the stack of flats above the
water that is placed in the bottom. A
wooden lid is used. Advantages: very
inexpensive; soil treated in containers.
Disadvantages: very small capacity; dif-
ficult to load and unload; does not fit
into mechanization. Best use: very small
nursery, home garden, or hobby green-
house.
13. Horizontal-tank type . . .
is a variant of the multipurpose tank
(type 7), apparently little used in this
country. Two modifications are used in
England. In one the tank has water in
the bottom and either soil in bulk or in
containers supported in stacks over it;
heat is applied from beneath by coal,
oil, or electricity. In another type, the
tank is mounted on wheels for porta-
bility, and has in the understructure a
coal-fired furnace to heat the water in
the tank. Reference: Lawrence and New-
ell (1950, p. 85-87, 145-57).
Dry Source of Heat
Thermal transfer from dry heaters to
a stationary soil mass is effected in one
of two ways.
1. If the soil is dry there is slow and
inefficient transmission from particle to
particle, the air spaces between acting as
insulation. It is necessary, therefore, to
use high temperatures for long periods
to get penetration of heat, and this usu-
ally means that the soil is excessively
heated at the point of contact, with char-
ring of the organic matter.
2. If the soil is moist, the soil water
at the heat source is converted to steam,
which moves outward in a zone, as ex-
plained in Section 9. It is evident, how-
ever, that in the zone where the moisture
has been evaporated, the soil will be
heated to excess, as in the case above.
There is an outer moving zone of steam,
followed by an inner expanding sphe-
roid of drying soil, and at the center an
area of very high temperatures (not un-
commonly reaching 400° to 500° F in
electric heater types) and charred or-
ganic matter. If continued long enough,
the mix would be entirely desiccated and
perhaps charred.
14. Box with electrical heating
elements in soil . . .
is now less commonly used than before.
Also called the New York, immersion, or
indirect type; it has been known since
L931 . It consists of a wooden box similar
to the steam box (type 4a above) in
r i7<> i
which are mounted special electrical
heating elements (fig. 89). These heavy-
duty immersion heating elements are of
the strap, plate, or rod types. Current
consumption about 1 to 1.5 k.w.h. per
cu. ft. The "cold" edges and bottom
four corners should be fitted with tri-
angular pieces of wood to expedite uni-
form heating. A small (Va cu. ft.) tubu-
lar model with single central heating
unit is used in England by amateurs and
gardeners. Advantages: simple, safe op-
eration; constant power load; quite ef-
ficient; inexpensive to build. Disadvan-
tages: requires quite moist soil to func-
tion without burning; chars organic
matter next to heating elements; uneven
heating; expensive to operate; used for
bulk soil only, with containers untreated;
very slow heating; does not fit well into
mechanization. Best use: in small nurs-
eries with other means of treating con-
tainers, but without steam source. Ref-
erences: Newhall (1940, p. 5-8, 14-18) ;
Hardy and Dillon, Inc. (1953) ; Brown
and Wakeford (1947).
15. Electrode type with soil heated
by resistance to electric current . . .
sometimes called the Ohio or direct type,
is seldom used in California, but ap-
parently is in England. It has been avail-
able since 1921. It consists of a box
similar to the steam box (type 4a), in
which are mounted metal electrodes
(fig. 90). The current passes through
the soil solution between electrodes due
to the presence of dissolved salts, gen-
erating heat in the soil in the vicinity of
the plates as a result of the resistance
presented. Current consumption varies
from 1 to 4 k.w.h. per cu. ft. of soil. A
transformer is required for best results.
Soil is dried in treatment. In England
a harrow-type grid of rod electrodes has
been successfully used, with a trans-
former, on ground beds; this required 3
to 4 k.w.h. per cu. ft. to reach 158° F.
Advantages: shuts off automatically at
180° to 200°, as water boils away from
electrodes; relatively uniform heating.
Disadvantages: serious shock hazard;
transformer is usually necessary and
makes equipment expensive; current
load varies widely as soil dries along
plates, with firmness of soil packing,
temperature, and with salt content of
soil; in some areas (probably not in
California) addition of epsom salts or
potassium nitrate is necessary; difficult
to insulate, particularly in ground beds;
not adapted to mechanization schedule.
Best use: little used; suitable only for
small nursery. References: Canham
(1951) ; Newhall (1940, p. 3-5) ; Taver-
netti (1935).
16. Box type with soil heated by
electrical induction grid . . .
has very rarely been used. It consists of
a box similar to the steam box (type
4a), in which an iron pipe grid enclos-
ing coils of copper wire is buried in
soil. Alternating current passes through
the coils, sets up currents in the pipes,
heating them. Advantages: as in type
14. Disadvantages: high initial cost;
localized heating, as in 14; insulation of
wire deteriorates; not adapted to mech-
anization program. Best use: limited to
small nurseries. Reference: Newhall
(1940, p. 13-14).
17. Baking or burning of soil . . .
an ancient method, is now obsolete be-
cause it is inefficient and destroys the
soil organic matter. Since organisms are
more resistant to dry than to moist heat,
the biological efficiency is low. Because
of low heat conduction by soil this
method is expensive and inefficient. Usu-
ally soil is placed in containers in an
oven, but in England special brick struc-
tures are used. Not recommended. Ref-
erence: Bewley (1939, p. 22-27).
[177]
STATIONARY SOIL MASS IN BENCHES OR BEDS
The preceding seventeen types, as well
as types 27 to 35, treat soil in bulk or in
containers. Nurserymen frequently must
treat soil in benches or beds, and the
methods now to be discussed have been
used for this purpose. Surface or pan
types (types 18, 19, 24) heat the soil
downward from the surface, whereas
buried pipes or tiles, or the spike or rake
methods (types 20 to 23) heat upward
from the bottom. It is reasonable, and
is supported by abundant experience,
that the buried-pipe or -tile or the mov-
ing-rake methods give the deepest soil
treatments. Where penetration below 8
to 9 in. is not required, the Thomas
method (type 18) may be used, but
where penetration to 12 to 18 in. or more
is required, the buried-pipe or -tile or
moving-rake method is necessary.
Pressureless Steam from External
Source Released around Soil
18. The Thomas or surface
method of steaming . . .
(fig. 91) has been widely adopted in the
past 13 years in this country and abroad.
A canvas hose, aluminum pipe, metal
downspout, perforated pipe, or simply
a series of croquet wickets set in the
soil, is placed lengthwise on the top and
center of the bed to be steamed. Over
this is spread a plastic sheet (Visqueen,
Duratex, Stericover, Velon Fumicover),
rubberized cloth, treated fabric (Fiber-
thin, Tufedge) , treated fiberglass (Steril-
tex), or paper (Sisalkraft) . These may
be fitted and tied around glasshouse
posts, or two strips may be laid length-
wise and joined at a wire stretched down
the line of posts, by folding the edges
together and clipping with spring-type
wooden clothespins (fig. 91). Sonic of
* One of the types considered best for Cali-
fornia conditions.
the materials automatically seal them-
selves to the sides of the bed with the
condensate ; others may be held down by
2x4 timbers (hot metal angle iron or
pipe may injure some plastics) placed
on top of sideboards. Wood strips may
also be held by C clamps against the ma-
terial on the inside of the sideboard, but
this reduces effectiveness of treatment of
sides. Lath may be tacked over the ma-
terial to the outside of the sideboards.
The arrangement should be nearly
steamtight and arranged so that it may
inflate with steam to a height of 5 to 6
in. Steam should be turned on slowly to
avoid blowing off the cover. Covers may
be used many times if properly cared for.
Plastic covers should not touch hot steam
pipes and should not be exposed un-
necessarily to sunlight, nor stored wet.
These covers act like a metal inverted
pan (type 19). The soil should be
loosened to the bottom of the bench or
the desired depth of penetration, and be
in good planting condition, free of clods.
The end of the bench where steam is in-
troduced may be difficult to heat because
of condensed water expelled there from
the pipes, or because of a dead air
pocket. The condensate and moist steam
should be drained from the pipes before
attaching the hose. A short perforated
side pipe from the main at this point will
provide steam distribution at the input
end. The cover should be left on for 30
min. after a final temperature of 180° to
212° F is reached. The method may be
used with free-flowing, pressure, or
superheated steam, operating in all cases
without pressure in the soil.
The method may be modified to treat
bulk soil in the headhouse. Pile the soil
7 to 8 in. deep on floor or workbench,
cover with tarp and place boards on the
edges to hold it down, then handle as
above. It may also be used for soil in
[178]
89
90
Fig. 89. Box type of heater, using electrical heating elements immersed in the stationary bulk
soil (type 14). Fig. 90. Electrode heater, in which the stationary bulk soil is heated by resistance
of the soil to passage of electrical current (type 15). Fig. 91. The Thomas or surface method of
steaming a bed of soil (type 18). The same method may be used for steaming soil in containers
(type 5).
[179]
Hats or pots, stacked with separators, in
the same way (type 5).
Another variation has been used for
ground beds in lath houses. A flat frame-
work of 1 x 4 lumber is placed on the
ground and covered with Velon. The
cover is held down with 2x2 lumber
clamped to the frame. Steam is released
under the cover through a canvas hose.
To move the unit, the steam is shut off
and the structure skidded by pulling it
with attached ropes, so that it slightly
overlaps the previous setting. The boards
are then pressed down into the soil. It
is not necessary to walk on treated soil
in this operation.
Advantages of the Thomas method:
simple, inexpensive, with parts readily
available; light labor requirement; effi-
cient; best practical way of treating
around posts and irregular areas; only
slight danger of getting burned in mov-
ing sets; permits treating field soil with-
out walking on it. Disadvantages: ap-
parently effectiveness below 8 in. is not
dependable; covers wear out (particu-
larly if of paper) ; some difficulty in
moving covers to new beds. Best use:
excellent for all bench treatment under
glass or outdoors; less effective on
ground beds requiring treatment depth
beyond 8 in. References: Dimock and
Post (1944) ; Seeley (1954) ; Ball (1953
[5]: 1-5; 1954).
* 19. The inverted-pan method
of surface steaming . . .
has been in successful general use for
about 60 years. The pan (fig. 92) is
best made of aluminum alloy or other
metal, is 6 to 9 in. deep, and of a size
determined by the size of beds, ease of
handling (by hand or with mechanical
aids), and by boiler size. The pan is
pressed into the ground 4 to 5 in. and,
if high-pressure steam is used, may re-
quire weights to hold it down. Soil must
l>c well worked up. of good planting
* One <»f the types considered best for Cali-
fornia conditions.
moisture, and free of clods. Tempera-
ture may be brought to 180° to 212° F
at 8 to 9 in. if soil is well worked up, but
does not penetrate a firm soil layer. Pan
is left 30 min. after reaching tempera-
ture, or it may be moved to next posi-
tion (overlapping the former) and the
hot soil covered by rubberized canvas
to hold in heat. About 2.7 sq. ft. per hr.
per boiler horsepower have been treated
with the pan method. If pans are to be
used in benches or beds, both should be
designed for the most efficient size and
proper fit. Pans may be used with free-
flowing, pressure, or superheated steam,
operating in all cases without pressure in
the soil. Advantages: simple, inexpen-
sive; efficient; soil not handled after
treatment, as in the case of types 20 and
21. Disadvantages: difficult to work
around posts or in irregular areas; dif-
ficult to move large pans (mechanical
aids are available — see Newhall, Chupp,
and Guterman, 1940) ; danger of getting
burned while moving pans. Best use: ex-
cellent for bench or bed treatments under
glass or outdoors. References: Newhall,
Chupp, and Guterman (1940, p. 24-
30) ; Newhall (1930, p. 31-39).
Pressureless Steam from External
Source Released into Soil
20. The buried-perforated-
pipe method . . .
a development from the Rudd type, en-
joyed long popularity but is now less
used because of the labor requirement.
Modified forms, the "Hoddesdon pipe" in
England and the "long pipe" in Europe,
are extensively used, but probably will
not replace the simpler Thomas method
here. About 2Vi> sq. ft. per hr. per boiler
horsepower have been treated by the
pipe method. Pipes 1 in. in diameter
with %-in. holes 9 in. apart, are laid 9
in. apart and 9 to 15 in. deep. Morris
(1954) found that the cross-sectional
areas of the pipe should be 1 Vi2 to 2
limes that of all the holes in it to insure
[180 |
Fig. 92. The inverted-pan method of surface steaming of soil in benches or beds (type 19).
This unit may be fitted with a water pan and electric heating elements, to make a self-generating
unit (type 24). Fig. 93. The buried-perforated-pipe method of deep steaming of soil in benches
or beds (type 20). Fig. 94. The spike method of deep steaming of soil in benches or beds (type
21). The pan covering the soil surface is to increase efficiency. Fig. 95. Permanent buried tile
method of deep steaming of soil in benches or beds (type 22).
[1811
uniform flow of steam to all of them.
The distance between pipes should not
exceed the depth they are buried by
more than 25 per cent. They may be
single or joined in a grid framework
(fig. 93). Pipes should be buried in
trenches in well-worked, clod-free, mod-
erately moist soil, and covered with rub-
berized canvas. When the temperature
is reached, pipes are pulled out and
moved to the next setting, and the hot
soil covered with a tarp. One Virginia
grower uses perforated 2-in. aluminum
downspout for the buried grid in out-
door beds. Winch-drawn adaptations
called "steam plows" are used in Den-
mark and England, which eliminate
digging up the pipe for each new setting.
Buried pipes may be used with free-
flowing, pressure, or superheated steam,
operating in all cases without pressure in
the soil. Advantages: deep treatment of
Fig. 96. The moving-rake method of deep-steaming a field soil (type 23). The rake is pulled
by a winch at the end of the field, the slanted blades penetrating to 14-in. depth. Fig. 97.
Device for heating water with steam as it is injected into the soil (type 25).
[182]
soil: very efficient use of steam. Disad-
vantages: high labor cost in burying and
digging up pipes: soil must be handled
after treatment, with recontamination
hazard: danger of getting burned while
moving grid. Best use: ground beds re-
quiring deep penetration. References:
Xewhall. Chupp, and Guterman (1940,
p. 21-24); Morris (1954, p. 11-13);
Bewley 1 1939, p. 4-11 I : Xewhall (1930.
p. 26-29); Schmitz (1954); Coates
(1954); Hansen (1953-54); Lawrence
(1956, p. 119-20).
21. The harrow, spike, or
rake method . . .
is now little used. It consists of a risid
pipe frame with vertical teeth on the
lower side, which are plunged into soil.
Steam is released through holes near tip
of each tooth. In England this is
mounted in a steam pan to reduce steam
loss (fig. 94). Morris (1954) found that
the space between pipes should not ex-
ceed the depth of steaming by more than
about 25 per cent, and that the spacing
of spikes along the pipe should about
equal the depth of treatment. The pipe
cross-sectional area should be IV2 to 2
times the area of the holes fed bv it to
insure uniform distribution of steam. A
single pipe with vertical teeth, called a
comb type, is also used in England. May
be used with free-flowing, pressure, or
superheated steam. Advantages: rapid
and easy to use: inexpensive; fairly ef-
ficient use of steam, particularly when
enclosed by a pan. Disadvantages:
serious steam "blow out" along spikes;
holes plug with soil: awkward to move:
danger of getting burned while moving
grid. Xo longer recommended. Ref-
erences: Xewhall (1930, p. 29-31);
Bewley (1939, p. 11-12. figs. 6-7):
Lawrence (1956, p. 109-10).
22. Permanent buried-tile
method . . .
has clay drain tiles buried end to end
in ground beds 13 to 16 in. deep and in
rows 18 in. apart 1 fig. 95). Tile is left
permanently in place; used for deep
steaming, as well as drainage, leaching,
and subirrigation. Tiles may be placed
in benches for steaming and then re-
moved, but this is too laborious, and
exposes the treated soil to handling. Soil
is covered with rubberized canvas dur-
ing steaming. About 1.3 sq. ft. per boiler
horsepower per hr. have been treated.
The connecting hoses should be removed
when the steam is shut off, to prevent
mud being sucked into the line as the
steam condenses. May be used with free-
flowing, pressure, or superheated steam,
operating in all cases without pressure in
the soil. Advantages: triple-function
permanent installation; gives deep soil
treatment. Disadvantages: very high
initial cost; laborious installation; soil
profiles disturbed; tiles must be reset
after several years to remain functional.
Best use: permanent ground beds under
glass or lath. Reference: Xewhall, Chupp,
and Guterman 1 1940, p. 11-21).
23. The moving-rake method . . .
has recently been introduced in Florida
for use on outdoor beds. The rake con-
sists of a 4-in. header 121//o ft. long, on
which are mounted, at 10-in. intervals,
blades 16 in. long, set on a 20° forward
angle (fig. 96). Descending immediately
behind each blade, and bent to trail 14
in. to the rear at blade depth, is a 12^n-
steam pipe connected to the header. As
the unit is pulled steadily forward by a
motor-driven winch, the blades dig in.
Forward progress is at about 25 ft. per
hr.. treating about 320 sq. ft. (370 cu.
ft. ) per hr., nearly 3 sq. ft. per boiler
horsepower. A trailing canvas skirt
covers the treated soil for about an hour,
maintaining the temperature to a depth
of 14 in. An adequate stationary, high-
pressure boiler provides the steam,
which is carried, preferably over the
untreated soil ahead of the unit, by a
2-in. steam hose. Could also be used with
free-flowing or superheated steam or
[183]
with steam-air mixtures. This unique
method has many possibilities of devel-
opment. It is suggestive of the winch-
drawn "long-pipe" method (a buried-
perforated-pipe type; type 20) used in
Denmark and England. Advantages:
deep treatment of field soil much easier
than with buried perforated pipe; very
efficient use of steam; cost per acre ap-
parently no greater than for some fungi-
cidal treatments. Disadvantages: initial
cost of equipment; large steam boiler
required; has moving parts to be main-
tained; slow operation. Best use: field
beds for high-valuation crops. Refer-
ences: Ball (1955); Coates (1954);
Anonymous (1955, 1956, 1957); Web-
ber (1956).
Pressureless Steam from Built-in
Generator Released around Soil
24. The electric-inverted-pan
method of surface steaming . . .
is a steam pan (type 19, fig. 92) with an
enclosed tray of water which is boiled
by electric heaters. Uses about 1.8 k.w.h.
per cu. ft. of soil. Advantages: much as
for type 19. Disadvantages : messy opera-
tion; high cost of electricity; limited to
small operations because of power load;
expensive heavy wiring required in glass-
house; overheats soil under electric
elements. Best use: small nursery using
no bulk soil or containers, and without
a steam source. Reference: Newhall
(1940, p. 25-30).
Hot-Water Drench of
Propagating Sand
Hot water transfers a maximum of
only 152 B.t.u. per lb. to soil at 60° F,
whereas steam yields 970 B.t.u. per lb.
at 212°. Thus, at least V/2 to 2 gal. of
water per cu. ft. of dry sand is needed in
order to raise the temperature from 60°
to 180°.
Hot-water drenches of propagating
sand leach out accumulated salts and, if
continued until the sand reaches 180° F
and remains at that temperature for 30
minutes, will destroy pathogens. If the
necessary quantity of water to do this
is troublesome, the sand may be leached
and then treated with steam.
25. Equipment for converting
steam to hot water . . .
as it is applied to the bed is available
(fig. 97), or hot water directly from a
hot-water boiler may be used. Advan-
tages : method is useful when only a hot-
water boiler is available; leaches sand
of soluble salts; may be used where
steaming gives toxic effect. Disadvan-
tages: extremely messy; not entirely de-
pendable; if used on soil, may puddle it;
not used on ground beds unless very
well drained. Best use: sand in propagat-
ing benches. Reference: Ball (1942,
p. 12-16, 19, 23-25).
Combined Steam and
Formaldehyde Vapor
26. Equipment to volatilize water
and formaldehyde . . .
was described 19 years ago, but has been
little tested. It is possible to drive formal-
dehyde as deeply into soil as the steam,
with increased effectiveness or shorter
required treatment time and reduced
cost of treatment. Most seeds may be
sown within 24 hr., and the necessity of
seed treatment is reduced because of the
slight soil residue. Formaldehyde is
added to water at rate of 1 pint per 40
to 80 gal. (0.4 to 0.2 fl. oz. per gal.) in-
jected into flash-type boiler or into the
steam line, and the vapor passed into 200
sq. ft. of soil; with steam pan this will
penentrate to 10 in. depth. Growers near
Toledo, Ohio, have injected formalde-
CAUTION:
Many
of
the <
:hemicals
mentioned
in this
manual
are
poi-
sonous and
may
be
harmful.
The
user should
carefu
lly
Follow the
pre-
cautions on
the 1
abe
Is of
the
con-
tainers.
184]
hyde into the steam line leading to per-
manent buried tiles in ground beds. They
reported decreased time and cost, and
increased efficiency over steam alone.
This system has many possibilities, and
should be further explored. The prin-
ciple involved is discussed in Section 9.
Advantages: cheaper treatment than
steam alone. Disadvantages: cannot be
used near living plants; may delay use
of soil; special boiler or accessories re-
quired. Best use: outdoor ground beds,
or in houses completely emptied of
plants; much experimental work needed.
Reference: Beachley (1937); Anony-
mous (1940).
More recently Thomas began studies
on the combined action of methyl bro-
mide and steam against nematodes.
Reference: Thomas (1954).
MOVING SOIL MASS IN CONTINUOUS OUTPUT
Because this type of treatment equip-
ment applies heat to a moving soil mass,
it is possible to terminate the process at
any desired temperature by varying the
heat input (through controlling the
steam, electricity, gas, or oil) or the time
of exposure (through regulation of the
speed with which soil is moved). The
principal disadvantages also arise from
this feature: power is required for the
soil movement; higher cost initially and
in maintenance of moving equipment;
greater risk of breakdown due to mov-
ing parts; lower heat-transfer efficiency
because of losses to air during move-
ment.
Pressureless Steam from External
Source Released into Soil
In this type of equipment the steam
condenses more or less uniformly on the
soil particles as they are tumbled about
until their temperature reaches 212° F.
From that point on the steam simply
escapes to the surrounding air, and the
soil temperature is not raised above
212° if continued longer.
27. The continuous-knife-injector
type for flats . . .
in which flats of soil are pulled under
the injecting knives, was designed by the
Department of Agricultural Engineering,
University of California. Davis. Though
not much used, this represents an inter-
esting new approach to soil steaming
(fig. 98) . The knives slice the soil in one
direction as the flats are pulled under
them, then a second set cut across the
flat as it is drawn at right angles. Power
is supplied by moving belts driven by an
electric motor. Advantages: soil treated
in containers; continuous operation;
uses efficient external steam source;
fairly efficient use of steam. Disadvan-
tages: small output; expensive to build;
power cost and mechanical upkeep of
moving parts; cannot be used for bulk
soil; probably insufficient soil volume
for mechanized schedule. Best use:
small bedding-plant nursery.
28. The horizontal-rotating-
drum type . . .
with steam released into the soil mass by
knife injectors is a possible variant of
type 30. The drum rotates on four rollers
and is driven by a large sprocket and
chain much as in type 30; in fact the
basic machine of that type (available
without burner) could well be modified
for this. Soil is fed in through a hopper
at one end, is carried through the ro-
tating drum at a rate controlled bv the
adjustable slope. In the center of the
drum is placed a steam pipe on which
are welded at right angles, 10 to 12 in.
apart, flat hollow knives of sufficient
[185]
Fig. 98. The continuous knife-injector steamer for moving flats of soil (type 27). Fig. 99. The
horizontal rotating-drum type of steamer with knife injectors (type 28). A continuous flow of bulk
soil passes through the drum and into flats or other containers.
[186]
length to reach nearly down to the drum
(fig. 99). These slice through the tum-
bling soil and inject steam into it. The
steam pipe is closed and welded to the
hopper at the input end, and the open
end is fastened to the frame at the other
end of the drum. The steam is obtained
from an external boiler, and may be of
the free-flowing, pressure, or super-
heated type. Some concrete mixers used
for mixing nursery soils might be fixed
with similar steam pipes. Advantages:
continuous operation; heat can be con-
trolled to any level above 160° F de-
sired, by varying time in drum; steam
is the heat source; may be used for
simultaneous treating and mixing of
soil; fits well into mechanization sched-
ule. Disadvantages: containers not
treated; initially expensive; power cost
and mechanical upkeep of moving parts.
Best use: if different sizes were available
would be useful in many nurseries re-
quiring bulk soil.
Pressureless Steam from External
Source Released around Soil
*29. The rotating-screw type . . .
for propulsion of soil through a pipe
into which steam is injected. A com-
mercial unit of this type is available in
California. Gas or butane burners gener-
ate steam in a tank beneath the soil pipe ;
the steam bathes the pipe and is intro-
duced into it through holes in the input
end of the shell. The soil is propelled
through the pipe by a screw rotated by
an electric motor (fig. 100). Advan-
tages: continuous operation; steam is
heat source; degree of soil heating con-
trollable; fits fairly well into mechaniza-
tion. Disadvantages: containers not
treated; initially expensive; power cost
and mechanical upkeep of moving parts;
propelling screw may wear badly. Best
use: general nursery use for providing
:,: One of the types considered best for Cali-
fornia conditions.
bulk soil.
(1953).
Reference: Anonymous
Dry Source of Heat
In equipment with a moving soil mass
and dry heaters the soil particles are
tumbled about so that they are heated
uniformly by direct transmission during
contact with the heating element. The
heating is uniform through the mass,
whether the soil is moist or dry. With
dry soil there is some transmission from
particle to particle when not in contact
with the heat source, and this makes for
uniformity through the mass. In moist
soil there is the additional heat transfer
by steam produced from water films
around particles in contact with the heat
source. This steam condenses on cooler
particles, heating them uniformly. When
all particles reach 212° F, the steam
escapes to the surrounding air; if long
enough continued the soil is desiccated.
With either situation there is no danger
of charring organic matter unless treat-
ment is continued beyond 212°.
30. The horizontal rotating drum
with internal blowtorch . . .
also called the flash-flame pasteurizer, is
used in the eastern states. It consists of
a rotating drum of adjustable slope, into
which soil is thrown at the high end,
coming out at the low end. Into the drum
from the low end is introduced a flame
from a large kerosene blowtorch, which
heats the soil (fig. 101) . The commercial
unit is said to use 2% to 6 gal. of kero-
sene per hr. and to turn out about 2 cu.
yd. of soil per hr. at 175° to 190° F. A
possible modification of this equipment
(see type 28) answers most of the dis-
advantages. Advantages: light weight,
portable, convenient; continuous opera-
tion; temperature of soil controllable by
varying time in drum; fits fairly well
into mechanization program. Disadvan-
tages: containers not treated; kerosene
flame directed into soil may leave an
oily residue which is injurious to some
[187]
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— W
^ vl ^c c c u c k j^nr
*M***y *M****p M»**M W^M WWI¥
a
^
^^^
100
Fig. 100. The rotating-screw type of steamer, continuous bulk output and self-generating (type
29). The steam prevents overheating in the tube, and is injected into the unit at the soil-input
end. Fig. 101. The horizontal rotating drum heater with internal blow torch (type 30). The bulk
soil is thrown in at one end, comes out continuously at the torch end.
188 1
102
&m_
^^
103
104
Fig. 102. The electric hot-plate soil heater giving a continuous output of bulk soil (type 32).
Fig. 103. The rotating screw type of electric soil heater (type 33). A continuous flow of bulk
soil is supplied. Electric heating elements are wound around the tube. Fig. 104. Method of stack-
ing flats of soil to permit unrestricted steam flow without the use of separator strips.
[189]
plants (this might be avoided by using a
gas flame) ; power cost and mechanical
upkeep of moving parts; dries soil. Best
use: small nursery using bulk soil and
having some means for treating contain-
ers; should first check for possible resi-
dual toxicity to the crop bsing grown.
Reference: Newhall and Schroeder
(1951).
31. The horizontal rotating drum
with external flame heat . . .
has been little used. It consists of a
rotary drum (sometimes an oil drum
with the ends removed), through which
the soil moves; heat is applied as gas or
oil flame to outside of drum. Advan-
tages: continuous operation; tempera-
ture of soil controllable by varying time
in drum; moderate initial cost; may be
used for simultaneous mixing and treat-
ing of soil; fits fairly well into mechani-
zation. Disadvantages: containers not
treated; power cost and mechanical up-
keep of moving parts; dries soil; small
capacity; heat torsion of drum. Best
use: small nursery needing bulk soil and
having means of treating containers.
32. The electric-hot-plate type . . .
has been used in New York, where it is
called the Hutchings type. Soil is pro-
pelled by a chain drive in a thin layer
along an elongated electric hot plate;
it is fed into a hopper at one end and
drops out at the other (fig. 102). Uses
about 1.5 k.w.h. per cu. ft. of soil. In-
frared lights have been used to impart
additional heat to the soil moving on the
plate; they would not provide sufficient
heat by themselves for the purpose. Dia-
thermy has been suggested, but the
energy available is also insufficient for
this purpose. Advantages: continuous
operation; uniform, controllable, rapid
heating. Disadvantages: dries soil; con-
tainers not heated; small capacity; high
cost of electric power (but could be op-
erated with gas burners) ; power cost
and mechanical upkeep of moving parts;
no stones or lumps can be tolerated;
capacity too low for effectively mecha-
nized nursery. Best use: small nursery
requiring only bulk soil and having
means of treating containers. Reference:
Newhall (1940, p. 30-32).
33. The rotating-screw type
with electric heat . . .
has been little used. It consists of a 4-in.
pipe 6 ft. long wound on the outside with
electric heating elements and housed in
an insulating shell (fig. 103). A revolv-
ing screw forces the soil from the hopper
at one end through the tube and out at
the other end, about 2 min. being re-
quired. Uses about 1 k.w.h. per cu. ft. of
soil. Advantages: continuous operation;
uniform heating of soil; efficient use of
heat; temperature controllable by chang-
ing speed of screw; moderate initial cost.
Disadvantages: soil containers not
treated; power cost and mechanical up-
keep of moving parts; sticks and stones
must be removed from soil; screw
wears badly; high cost of electric power;
necessity of power wiring; dries soil;
small capacity (4 to 7 cu. ft. per hr.)
limits use in mechanization program.
Best use: small nursery using bulk soil
and having means of treating contain-
ers. Reference: Tavernetti (1942).
34. The rotating-screw type
with external gas heat . . .
has been little used although a com-
mercial unit was available for a time.
The pipe, through which the screw
forced the soil, was heated by a gas or
oil flame. Advantages, disadvantages,
and use as for type 33; heat produced
torsion of equipment.
90
MOVING SOIL MASS TREATED IN BATCHES
Dry Source of Heat
35. The horizontal rotating drum
with external flame heat . . .
has recently been introduced as a com-
mercial unit in the eastern states. It con-
sists of a drum which holds about l1/^
cu. ft. of soil. Soil is tumbled during
heating, and the unit shuts off when soil
is heated. Uses bottled gas for fuel, and
treats about % cu. yd. of soil per hr.
at 180° F. Fuel cost said to be about
$1.10 per cu. yd. Advantages: final soil
temperature automatically controlled;
simultaneously mixes and treats soil.
Disadvantages: containers not treated:
power cost and mechanical upkeep of
moving parts; small capacity. Best use:
small nursery that has means of treating
containers. Reference: Tarrant Mfg. Co.
(1955).
EQUIPMENT FOR GENERATING AND DISTRIBUTING STEAM
Certain aspects of the generation and
distribution of steam having special ap-
plication to its use in soil treatment are
here discussed. For more detailed in-
formation consult standard reference
books on the subject, or a heating engi-
neer. Some of the principles involved
should be understood by the grower for
maximum results.
Types of Steam-Generating
Equipment
There are many kinds of boilers that
may be used for this purpose, but we
shall here consider some of their general
characteristics rather than specific types.
High-pressure versus very
low-pressure steam
It was customary up to about the last
decade to use high-pressure steam for
soil treatment, and many growers even
considered this to be essential for suc-
cess. Now, however, it is recognized
that: (1) such steam expands and the
pressure is lost when released into soil,
the temperature dropping to essentially
that of free-flowing steam; (2) steam at
80 pounds transfers only 36 B.t.u. (about
3.7 per cent) more heat per pound than
does free-flowing steam and is, therefore,
not a significantly more effective me-
dium of heat exchange (fig. 77); (3)
the principal benefits from high-pressure
steam are the faster distribution through
the pipes (see below), and the evapora-
tion of droplets of water through ex-
pansion of the steam during the drop in
pressure along the distribution line; (4)
the use of larger distribution mains
achieves the same improved flow without
the need of pressure. From these con-
siderations and from the experience of
many growers has developed the present
more economical practice, both in this
country and abroad, of using low-pres-
sure boilers with well-insulated mains of
suitable size and the shortest length pos-
sible.
There are other reasons for using low-
pressure equipment. Because such boil-
ers do not require heavy pressure-resist-
ing shells or pipes, they are less expen-
sive and lighter in weight. The distribu-
tion lines may also be of lighter con-
struction I although larger in diameter),
and there is less difficulty in making the
system steamtight. Water may be fed di-
rectly into low-pressure boilers from
water mains, and controlled automati-
cally by a float valve. If the boiler op-
erates at above 15 pounds' pressure
[191]
there may be operational restrictions im-
posed in some localities, and the boiler
insurance is somewhat more costly. Be-
cause of the higher temperature of steam
under high pressure (323.9° F at 80
lb.), there is more heat loss in the lines
than at lower pressures (227.1° F at 5
lb.), and greater insulation is required.
In some cases, low-pressure steam is
superheated to attain greater heat ex-
change (47 B.t.u. more per 100° F; see
fig. 77). Boiler costs may be about the
same or a little less than for high-pres-
sure steam. The lines must be larger and,
because of the higher temperature, well
insulated and as short as possible.
Furthermore, such boilers are not used
for heating glasshouses. For these rea-
sons, superheat boilers are used spe-
cifically for soil treatment. They may be
permanently located at the site of treat-
ment or may be portable, thus decreas-
ing the length of main.
Regular boilers versus
"flash" steamers
The so-called "package" and "flash"
steamers are small portable units that
include both boiler and burner, and de-
velop steam in a short period of time.
Generally they operate as free-flowing
units, water being injected into one end
of a pipe coil in a firebox, and steam
coming out the other at very low pres-
sure. The volume of steam may be large
or small, according to the size of the
unit. Types with a steam dome that
collects and returns some of the en-
trained water droplets are to be pre-
ferred to those in which the steam comes
directly from the end of the generating
pipe, since they supply drier steam.
Types that use part of the water in an
external jacket may be more efficient in
the use of heat. Such steamers are excel-
lent in small nurseries without other
sources of steam. The several types
presently on the market may be operated
on gas, oil, butane, propane, or elec-
tricity (see Apnendix). They are de-
signed for continuous output, and are
not used in return-type steam heating
systems. In southern California they are
subject to inefficiency due to rapid scal-
ing of the steam pipes from the high salt
content of some water, particularly be-
cause scale is collected from the large
volume of new (rather than recirculated)
water that is heated. In areas where scale
is troublesome it may be desirable to use
a water softener (Sec. 4). The "flash"
steamers are initially much less expen-
sive than regular types, but their useful
life is generally less.
There are many types of boilers on
the market, both new and secondhand.
These range from cast-iron sectional and
steel fire-tube boilers for small opera-
tions, to steel water-tube boilers for large
installations. They may be vertical or
horizontal types. They are usually in-
ternally fired (for example, steel firebox
and marine types), but may require
construction of an expensive external
brick firebox. Most of this type give long
dependable service in supplying steam
both for soil treatment and heating glass-
houses. Wherever practical such boilers
are preferable to less expensive package
units. With regular boilers, as with the
"flash" steamers, the problem of scaling
is increased when steam is bled from the
system for soil treatment rather than re-
circulated, as in a heating circuit.
It is possible to modify some (but not
all) hot-water boilers so that they will
generate steam for soil treatment. An
automatic water-level feeder, a 15-pound
safety valve, a water gauge, and a series
of valves are necessary. The water level
is lowered, and the upper part of the
boiler serves as a steam dome, or a
separate steam drum may be attached.
With cast-iron boilers, the injected water
should be preheated. Consult a heating
engineer for any particular installation.
It is usually better to run separate lines
for the steam than to try to use the hot-
water mains.
[192]
Stationary versus
portable units
Some types (for example, bricked-in
boilers) are completely nonportable.
Most other types may be portable in the
smaller sizes, but not in the larger.
Finally, the small "package" steamers
referred to above are designed for port-
ability. It is generally most convenient
to restrict the use of portable boilers to
small operations, or to divide the large
job up into small parts that can be han-
dled by such equipment. Both types of
operation have a definite place in the
California nursery industry.
Aside from the low initial cost, there
are other potential advantages in a
portable unit. With such a unit, the
large boilers need not be fired up for a
small soil-treatment job during warm
weather. The steam is generated at the
job rather than being conducted there
through mains (with loss of steam, and
increased steam condensation in the
process), or than taking the job to the
steam source.
In England it is possible to rent
boilers for soil steaming. Custom steam-
ing is done in England, Europe, and in
New York state. Some English growers
have also grouped together to purchase
a boiler, much as farmers in the eastern
part of this country have formed "spray
rings" to buy equipment for their or-
chard or potato spraying. Similar ar-
rangements might be advantageous
among smaller California nurseries. It
is possible that someone could operate
a profitable business supplying steam or
renting boilers to small nurseries. For a
number of years in southern California,
a complete portable service unit for
steaming soil in flats operated success-
fully in a number of nurseries. A possible
variation of this would be to provide
small nurseries with uniform soil bins
containing a pipe grid. When one was
empty, the nurseryman would refill it
with the desired soil mixture. He might
then have the operator steam the soil.
An additional kind of work available to
the operator of a portable boiler would
be the treatment of outdoor or lath-house
soil beds for nurseries, and even in home
yards (Sec. 8). Another variation would
be to have a centralized soil service
which would mix the specified soil and
place it in a dump truck with a per-
forated pipe grid (mobile bin; type 2)
which would be connected to a large
boiler for steaming. The soil would be
tightly covered with a tarp and delivered,
still hot, into the bins of the nursery,
much as ready-mixed concrete is today.
Variations of these types are operating
in England, and presumably could do so
here.
Size of boiler required
to steam soil
Because soil steaming may be done in
small or large quantity at each run,
there can be no general statement of
boiler size related to size of nursery.
When a boiler is used solely for steam-
ing soil, there is a fairly consistent re-
lation between the time required to do a
given job and the required size of boiler.
However, in nurseries using steam heat
there is a definite relation between size
of boiler and area to be steamed, and the
time required to do the job is more
uniform.
The question of the size of boiler re-
quired is related to the volume of steam
already discussed (table 14). Because
the requirements vary with soil moisture,
temperature, and type, with the over-all
efficiency of generation and distribution,
and with the distance from the boiler,
general figures may be quite misleading.
Furthermore, the rating of boilers in
horsepower may still be based largely on
area of heat exchange between the fire
and the water5 rather than on demon -
5 Even this method of calculation varies from
8.2 to 10 sq. ft. of heat-exchange area per boiler
horsepower.
[193]
strated production of pounds of steam
per hour. Because of these facts, the data
are quite variable. Newhall (1953) gives
l1/*? to 6 cubic feet of soil per boiler
horsepower per hour as the range in
commercial practice, with 3 cubic feet as
a working average. If one assumes that
each rated horsepower of a boiler gives
33.475 B.t.u., the over-all efficiency is
then only 28.2 per cent for the average,
and 56.5 per cent for the maximum vol-
ume of soil treated. Published figures by
other workers on commercial operations
fall within the above range of boiler
requirements. From these data it is pos-
sible to estimate the size of boiler that
will be required to treat a given area or
volume of soil in the permissible time.
The efficiency of the heat-exchange
system from boiler to soil is highly
variable. The boiler efficiency may range
from 40 to 90 per cent, and is the main
point of lost energy. There are further
losses of heat in the distribution piping,
these increasing with distance from the
boiler and with decreasing pipe size;
this may range up to or above 8 per cent
of the boiler output. There may be large
losses during injection of steam into
soil, from escaping vapor, heating of
structural material of beds, and so on;
loss may range from 9 to 56 per cent of
that introduced into the soil. Morris
(1954) calculated that an over-all ther-
mal efficiency of 41 per cent in the heat-
transfer system from coal to soil was a
good target for English growers effi-
ciently using present equipment and a
buried perforated-pipe grid; this would
represent about 68 per cent efficiency in
the part of the system; following the
boiler.
Table 14 presents data on the volume
of soil that can be heated per hour, and
the time required to heat I cubic yard,
for several boiler capacities and thermal
efficiencies. The efficiency of the boiler,
distribution system, and soil-injection
processes may be approximately calcu-
late! (see Appendix). Such data should
be useful in analyzing the heat-exchange
process for possible increased efficiency.
Type of Fuel or Power Used to
Generate Steam
Natural gas . . .
is the least expensive fuel in California,
but it is not always available without
excessive piping cost. It may be used for
stationary boilers but not for portable
ones, and should never be piped into a
glasshouse filled with plants in order to
operate a portable unit. It is sold on a
cubic-foot basis, each delivering 1,100
B.t.u.
Fuel oil .. .
is commonly used for steam boilers be-
cause it is fairly inexpensive. It requires
a storage tank and fairly expensive
burners, particularly for the heavier
cheaper oils. It is quite readily used in
portable units. It is sold on a gallon
basis, providing about 141,000 B.t.u.
per gallon for the No. 3 grade.
Kerosene . . .
is used by one commercial portable unit
for soil treatment (rotating-drum type
with internal flame; type 30), but is
otherwise not commonly used. It is sold
on a gallon basis, each yielding about
130,000 B.t.u.
Coal . . .
(bituminous) is used solely for sta-
tionary boilers in this country, and both
stationary and portable units in England
and Europe. It is both dirty and incon-
venient to use and requires a great deal
of attention, even with automatic stokers.
It is sold on a ton basis (2,000 lb.),
yielding about 14,000 B.t.u. per pound.
Butane . . .
is used where natural gas is not available
and the boiler is not equipped for oil. It
can be used for portable units. It yields
about 102,000 B.t.u. per gallon.
[194]
Propane . . .
or bottled gas, is usually the most ex-
pensive of the fuels. Uses as for butane.
It is sold on a gallon basis, yielding
91,800 B.t.u. per gallon.
Electricity . . .
is the most convenient, cleanest, and
most expensive source of power. Its use
is restricted to small boilers where for
some reason other sources of power can-
not be utilized, and to self-generating
soil-treatment units (types 10, 11, 14 to
16, 24, 32, 33). It is sold on a kilowatt-
hour basis, each k.w.h. yielding 3,411
B.t.u. Because of the heavy power de-
mands of any sizable unit, very heavy
wiring must be provided, and with some
units (for example, electrode type; type
15) a transformer may also be required.
Power requirements reported for the
various types of equipment range from
1.0 to 4.0 k.w.h. per cubic foot of soil,
with a working average of 1.5 to 2.0
k.w.h.
Distribution of Steam
The objective is to deliver the steam
at some distant point from the boiler
with a minimum loss of heat, pressure,
and rate of flow, and a minimum of
condensation. Among the many factors
that influence the flow of steam in the
pipes are the following.
Length of the pipe
Lengthening the pipe sharply in-
creases the rate of pressure drop and
heat loss. Thus, Morris (1954) calcu-
lated the heat loss for an uninsulated
1%-in. steel pipe carrying 25 lb. steam
per min. at 100 lb. pressure to be 3.1 per
cent at 100 ft., 5.8 per cent at 200 ft.,
and 8.3 per cent at 300 ft., the pressure
drop was 21, 46, and 95 lb. in the same
distances. A 21/^-in. uninsulated steel
pipe with 10 lb. pressure and the same
flow lost 2.3 per cent of its heat in 100
ft., 4.6 per cent in 200 ft., and 6.9 per
cent in 300 ft.; the pressure drop was
2.8, 5.9, and 9.3 lb., respectively. By con-
trast, an uninsulated 2^-in. aluminum
pipe carrying 25 lb. steam per min. at
10 lb. pressure lost 1.2 per cent of its
heat in 100 ft., 2.5 per cent in 200 ft.,
and 3.7 per cent in 300 ft.
Diameter of pipe
Increasing the diameter of the pipe
decreases the pressure drop and heat
loss; there may be a 4- to 6-fold increase
in the rate of flow by increasing the pipe
size from 1 inch to 2 inches. Senner
(1934) found, furthermore, that a main
used for soil steaming would carry ap-
proximately 4 times as much steam as
one of the same size used for glasshouse
heating. This was due to the free flow of
steam, unrestricted by the back pressure
of a closed system. This factor should be
considered if the mains are to be used
only for soil steaming, cannot be if they
also serve as heat mains.
Type of pipe
The kind of pipe greatly influences the
heat loss, as the above figures show.
Morris (1954) has suggested the use of
light alloy aluminum irrigation pipe for
steam mains in low-pressure systems,
because the heat loss is about half that
from steel pipe and it is much lighter
in weight. Such pipes, with light insula-
tion, are also used in the Scandinavian
countries for connecting portable boilers
to outdoor beds for steaming.
Steam pressure
The rate of flow increases approxi-
mately 4-fold with increases in steam
pressure from 10 pounds to 100 pounds,
with constant pipe size. The past practice
of using high steam pressure and rela-
tively small pipes is giving way to low
pressure and large pipes. The larger
pipe size does not increase heat loss
owing to the larger exposed surface, be-
cause this is offset by the lower tempera-
ture involved. If insulated aluminum
[195]
pipes are used the efficiency of steam
distribution will be greatly improved
over the old method (3.7 per cent heat
loss in 300 ft. against 8.3 per cent; see
above) .
Internal roughness of pipe
The flow of steam is decreased by the
internal roughness of the pipe and by
valves, elbows, tees, and reducers in the
line, since they increase the friction.
Quality of steam
Steam quality also affects the rate of
flow, decreasing it as the number of
water droplets increases. Since super-
heated steam is relatively drier than
saturated steam, it flows faster.
Water in the steam lines
Water condensation in the steam lines
should be prevented for the above
reasons, because it represents lost heat,
and because it affects the efficiency of
soil steaming. The condensed water car-
ried into the soil has a temperature of
212° F and, therefore, adds no heat; the
970 B.t.u. per pound (fig. 77) from the
steam has been lost in transit. Further-
more, the soil is made wetter than it
would otherwise be. The steam line
should always be drained and bled until
dry steam appears, before it is connected
to the treatment equipment. This will
prevent the injection of cold water into
the soil; in this connection it should be
recalled that it takes five times as many
B.t.u. to heat a pound of water as a
pound of soil. Furthermore, a water trap
should be placed in the line at a point
just preceding the treatment equipment,
the condensate either going into the re-
turn line or being wasted. If there is
considerable condensation in the line
this procedure becomes particularly de-
sirable.
Designing the steam
distribution system
Many of these factors can be resolved
for lines used solely for soil treatment
by operating the boiler at pressures be-
low 10 pounds, and using large, well-in-
sulated pipes (perhaps of aluminum
alloy) that are as short as possible.
However, if the pipe is too large, the
heat loss from the increased surface
exceeds that saved by reduced friction.
The losses may also be reduced by using
a portable boiler close to the soil being
treated. A heating engineer should be
consulted for the specific design.
SOIL TREATMENT IN A MECHANIZED NURSERY
Mechanization of every practicable
nursery procedure is of increasing in-
terest to the industry, due to rising wages
for labor and smaller margins of profit.
Any successful mechanized nursery pro-
gram must include, indeed must be built
around, soil treatment, for reasons out-
lined in sections 2 and 3. A number of
methods and pieces of equipment pre-
viously described for soil treatment
integrate very well into mechanized nur-
sery practice, and 13 of these are shown
schematically in figure 126. By following
the arrows in that figure, the routing of a
particular procedure may be visualized.
It should be emphasized that untreated
flats, cans, or pots may be used in the
procedure prior to soil treatment, but
that treated soil should not be dumped
into untreated containers or on an un-
treated floor (Sec. 12). Mechanization is
further discussed in Section 17.
[196]
SECTION
Chemical Treatment
of Nursery Soils
Donald E. Munnecke
Fungicides
Nematocides
Insecticides
Soil drenches around living plants
s
OIL may BE treated with chemicals
to rid it of fungi, bacteria, insects, nema-
todes, and weeds. The effectiveness of
chemical soil treatment generally de-
creases as the size of the treated area
increases. Although early trials of soil
fumigation in the field attempted to
eradicate pathogens and insects, experi-
ence has shown that this is impractical if
not impossible; a few chemicals are,
however, effective in reducing field in-
festations, and some of them are men-
tioned briefly in this section. On the
other hand, pathogens can be eradicated
from soil in containers such as flats,
where the chemicals do not need to
penetrate large soil masses. Steam treat-
ment is usually more satisfactory, but
there are many occasions where chemi-
cals can be used more cheaply and
effectively and their use has increased
tremendously.
The cost of chemical fungicide treat-
ment using methyl bromide or chloro-
picrin varies from approximately 1 to 3
cents per cubic foot, according to the
method and chemicals used (table 16).
The present practice is to use the chemi-
cal and dosage which will give the
greatest net return to the grower, as
determined by practical experience. It
is difficult to recommend single dosages
of chemicals for all soils and all condi-
tions. In general, the lower dosage
recommended herein is for use with a
U. C.-type mix; the higher dosages are
recommended for use on clay soils or
soils containing undecayed organic
matter.
An ideal chemical for treating soil is
one that kills a variety of fungi, bacteria,
insects, and weeds; is inexpensive and
harmless to the operator and equipment ;
is quick-acting and effective deep in the
soil as well as on the surface ; is harmless
to near-by plants; and is nontoxic to
subsequent plantings in the soil. None of
the presently known chemicals fulfills
CAUTION: Many of the chemicals
mentioned in this manual are poi-
sonous and may be harmful. The
user should carefully follow the pre-
cautions on the labels of the con-
tainers.
[197]
Table 1 6. Comparison of the Cost in 1 955 of Methyl Bromide and
Chloropicrin Used to Treat Soil for Fungus Control
Exclusive of labor and cost of accessory equipment
Cost
Dosage
Flats*
Bulk
Surface
Chemical
Cents per
flat
Cents per
cu. ft.
Cents per
sq. ft.
$1.65 per lb.
3 cc
1.8
1.8
(1-lb. lot)
5 cc
3.0
Chloropicrin
$1.25 per lb.
3 cc
1.4
1.4
(25-lb. lot)
5 cc
2.3
$1.02 per lb.
3 cc
1.1
1.1
(100-lb. lot)
5 cc
1.9
$0.80 per lb.
4 lb. per
(1-lb. lot)
100 cu. ft.
2.2
3.2
3.2
Methyl bromide
$0.72 per lb.
4 lb. per
(50-lb. lot)
100 cu. ft.
1.9
2.9
2.9
* Chloropicrin not recommended for flats. Flats 18 X 18 X 3 inches. These figures based upon 40 flats
per cu. yd. of air space. In actual practice the cost varies with the way the flats are stacked and the dosage
used. The dosages given are sufficient to eradicate pathogens in confined areas. The lower dosage of chloro-
picrin is sufficient for this purpose with a U.C.-type mix; the higher dosage may be necessary for clay soils
or those high in manure or other undecayed organic matter.
all of these requirements, but many ful-
fill enough of them for practical use.
Much research is being done on this
problem and it is probable that some
materials will be available in the future
that approximate this ideal. The most
common chemicals, dosages, and treat-
ments used to control diseases and nema-
todes in nursery soils are summarized in
table 17 at the end of this section.
Special chemicals and dosages
required to kill fungi
Fungi, such as Rhizoctonia, Fusarium,
Armillaria, and Verticillium are, in gen-
eral, more difficult to kill in the soil with
chemicals than are insects, nematodes,
and most weed seeds. This fact must be
kept clearly in mind when a chemical is
chosen for soil treatment. For example,
it is a waste of time and money to use
ethylene dibromide, an excellent noma-
tocide, to try to control damping-off,
which is caused by fungi. Also, low
dosages of methyl bromide, an excellent
soil fungicide, may be used for weed
and nematode control, but two to four
times as much may be required for fun-
gus control. Growers often erroneously
believe that if weeds and nematodes are
controlled, the fungi are also. If fungi
are controlled, however, insects and
nematodes are usually eliminated. // the
main problem is fungus control, suitable
fungicides at recommended dosages must
be used. Nematocides or herbicides can-
not be used to control fungi.
Soil preparation, temperature,
and aeration
The condition and temperature of the
soil must be considered in using chemi-
cals for soil treatments. A good rule to
follow is that the soil should be in good
planting condition before treatment. The
soil should be in good tilth, and there
[198]
should be no lumps or clods. Too much
soil water prevents thorough diffusion
of the gas (Sec. 9), whereas too little
moisture on the soil surface allows the
gas to escape. Best results are obtained at
soil temperatures of 65° to 75° F. Where
soil is likely to be cold and wet for long
periods, chemical treatment may be
facilitated by storing it in bins in a
heated shed. It may then be treated in
place.
After treatment the soil must be
thoroughly aerated so that all trace of
the fumigant is gone before planting.
In general, the higher the temperature
and the lighter the soil, the shorter the
aeration period. In all cases the chemi-
cals should be handled with care, as
should any poisonous substance.
After-effects of treatment
In some cases an increased growth
response is apparent in chemically
treated soils (fig. 119). This is not be-
cause the chemicals act as fertilizers, but
probably because the soil-borne patho-
gens and pests are eliminated and a more
favorable balance of the other micro-
organisms is obtained (Sec. 14).
Occasionally soil treated with chemi-
cals is toxic to subsequent plantings. This
toxicity is usually due to insufficient
aeration of the soil after treatment. Soils
which are high in some organic ma-
terials or clay, excessively wet, or treated
at low temperatures may contain toxic
amounts of the chemicals several weeks
after application. These ill effects are due
to a residue of the gas, to a breakdown
product of it, or to secondary reactions
of soil microorganisms causing such re-
sults as ammonium accumulation. Usu-
ally this toxicity may be avoided by
applying the chemicals correctly and by
delaying planting until all odor of the
chemicals is gone. The use of a U. C.-type
soil mix greatly reduces the chance of
injury from chemical treatments, another
reason for adopting such a system.
Recently the chemicals containing
bromine (methyl bromide, ethylene di-
bromide, chloro-bromo-propene) have
been found to leave a residue which is
extremely toxic to certain plants (espe-
cially carnations) ; these compounds
should not be used on soil to be planted
to carnations. Although a large number
of bedding plants and other crops have
been planted in chemically treated soil
without harm, it is a good precaution to
use chemicals on a small scale on an un-
tried crop and note the results before
treating large quantities of soil.
Formaldehyde treatment
of floor
Whenever treated soil is dumped in
bulk piles on the floor, the surface should
previously have been wet down with a
formaldehyde solution (1 gal. to 18 gal.
of water) .
FUNGICIDES
A wide variety of chemicals is mar-
keted for soil treatment of one, sort or
another. The various chemicals are here
grouped according to the purpose to
which they are suited. First let us con-
sider fungicides.
The soil troubles caused by fungi are,
in general, the most difficult to control
with chemicals. Some fungi are able to
survive in soil for many years in the ab-
sence of their host plants. Most of them
form thick-walled resting bodies which
are resistant both to unfavorable en-
vironmental conditions and to chemical
treatments (Sec. 3) . A number are capa-
ble of growing or persisting deep in the
soil, well below the depths reached by
the surface treatments of the soil. The
most effective soil fungicides are fumi-
gants which act as gases in the soil.
[199]
Chloropicrin, methyl bromide, and
formaldehyde are the most widely used
soil fungicides. These compounds are
liquids whose gaseous phases diffuse
through soil. When properly applied in
adequate dosages, they control most of
the fungi, nematodes, and weeds. The
gases have to be confined in some way
during the treatment period. After treat-
ment the soil must be thoroughly aerated
before planting.
For sources of soil-treatment materials
in California see the Appendix. It is not
necessary to get a license to use these
chemicals.
Chloropicrin
Chloropicrin, or tear gas, is extremely
toxic to soil fungi, insects, weed seeds,
and nematodes. It penetrates bulk soil
readily, but does not readily penetrate
plant tissue such as unrotted nematode
galls. It is neither explosive nor in-
flammable, but it is difficult to use since
it is a potent tear gas.
To avoid eye irritation, start working
on the windward side of the planting
with the back to the wind so that the
fumes are carried away from the eyes.
Do not rub eyes when affected; rather,
turn and face the wind and let the effects
wear off. Since it is very corrosive to
most metals (but not to stainless steel),
metal equipment must be washed with
kerosene after using. It cannot be used
in the vicinity of living plants; conse-
quently, all plants in a glasshouse must
be removed before treatment. It may be
used in semienclosed areas, such as lath
houses, provided there is ample air
movement to dissipate the gas, and ad-
jacent plants are over 3 feet away from
the treatment area.
Heavy soil absorbs large quantities of
the gas and requires larger dosages and
longer aeration periods than light soil.
Chloropicrin may be applied by ma-
chines in field applications, or by hand-
operated injectors (fig. 105). For sur-
T
K>
1
Fig. 105. Hand-injector for applying soil fumigants, at left. Proper spacing shown at right
for hand-injection of fumigants into soil in beds, benches, or fields.
[200]
face applications the dosage is 3 cc per
12-inch square, injected 6 inches deep;
for bulk soils the dosage is 3 to 5 cc per
cubic foot. Bulk soils may be treated in
bins, drums, garbage cans, or any gas-
proof receptacle that can be tightly
sealed. The gas may be confined in fields
by wetting the top inch of soil or by en-
closing beneath a gasproof cover (poly-
ethylene types, such as Visqueen, are
most common) for 1 to 3 days. In gen-
eral, plantings must be delayed 7 to 10
days after treating or until all traces of
the gas have disappeared. Do not use
if soil temperatures at 6-inch depth are
below 60° F; best results are obtained
at 70°.
Chloropicrin is specifically recom-
mended in soil used for chrysanthemums
(dosage: 3 cc on 12-inch centers, 6
inches deep) and carnation plantings in
California, since methyl bromide is
sometimes unsatisfactory for these crops.
With proper application and aeration,
chloropicrin-treated soil gives excellent
disease control and plant growth, and it
is generally considered as the experi-
mental standard when comparing soil
fungicides. However, it is difficult to
handle, it requires much labor to apply,
and the treatment periods are long.
Aeration of the soil after treatment is
essential since a number of crops have
been lost through faulty aeration. Con-
sequently, it is not recommended for
flat-soil operations nor for other circum-
stances where soil must be used soon
after treating. See table 16 for approxi-
mate cost of chloropicrin.
Methyl Bromide
Methyl bromide is widely used, espe-
cially for flat- and bulk-soil sterilization.
It has been approved by the California
Department of Agriculture for treatment
of soil in which certain plants may be
grown if they are to be shipped, using
the Intercounty Nursery Stock Certifi-
cate or "pinto" tag (sees. 3 and 8). It is
effective against most of the soil pests,
is simple to use, and has the shortest
treatment and aeration period of the
present soil fungicides.
Although it is extremely toxic to man,
there is little danger if it is handled with
reasonable care. Take adequate precau-
tion to prevent exposure of children and
other persons to the poisonous gas. Post
warning signs.
It is marketed in several forms (pure
methyl bromide, methyl bromide with 2
per cent chloropicrin, or as a liquid in
various solvents), but the pure gas is
almost exclusively used in California and
the following recommendations apply
to this gaseous form.
Field soils, ground beds, flats, pots,
cans, tools, and even large trucks and
farm machinery may be satisfactorily
treated with methyl bromide by enclos-
ing them beneath a gasproof cover
(polyethylene is cheapest; polyvinyl
chloride and vinyl-coated nylon are
more durable, but more expensive) and
injecting the gas beneath the cover
through special applicators from cans
or cylinders (figs. 106 and 107). The
cover must be examined carefully for
holes; these may be sealed with masking
tape. The cover must be sealed tightly
with soil around the edges before apply-
ing the gas. Never use the gas at soil
temperatures below 50° F, preferably
around 70°. For treatment of contain-
ers see Section 12.
Treating stacks of flats
Up to 400 flats can be adequately
treated in one stack as follows.
Fill the flats with soil moistened in
preparation for planting, but not pud-
dled or rendered soggy. Place them on
a level surface or hard dirt area and
stagger them as shown in figure 107, or
use lath spacers between flats to allow
free circulation of the gas. Fasten the
outlet of a rubber or plastic hose to the
top of the center flat so that it points
away from the soil. Place burlap or rags
over the corners of the flats to prevent
[201]
damage to the cover. Put the cover
loosely over the top and seal the edges
with a dirt seal or with "sand snakes"
(canvas or plastic tubes 3 inches in di-
ameter filled with sand).
The gas may be more effectively ap-
plied by heating it in one of several ways
before injecting beneath the cover. The
simplest way is to immerse the cans in
a bucket of water heated to 140° to
160° F, or to route the gas through a
copper coil immersed in hot water (fig.
106) . If large cylinders are used, the gas
may be circulated through heated coils
in the same manner. A supplementary
heating device may be used to keep the
water hot.
Avoid turning cans upside down while
injecting. If cans are turned upside
down, liquid methyl bromide will flow
through the hose. This reduces effective-
ness and may cause the soil to be toxic
near the hose exit.
To calculate the amount of chemical
to use, multiply the length, breadth, and
height of the stack in feet, including the
air space beneath the cover. Use 4
pounds of methyl bromide per 100 cubic
feet for fungus control (damping-off,
root rot, etc.), or 1% to 2 pounds per
100 cubic feet for weed and nematode
control. A special metering device (fig.
106) is advisable for use on cylinders,
or a scale may be used to actually weigh
the gas as it is being dispensed. Place the
cylinder on a leveled scale, note its
weight, open the valve and allow the gas
to flow until the scale indicates that the
desired amount of gas has been used.
Close the valve and recheck the weight.
The initial weight minus the final weight
equals the weight of methyl bromide ap-
plied.
After a 24- to 48-hour treatment pe-
riod, remove the cover and allow the
flats to aerate for 24 to 48 hours, when
they are ready for planting.
Fig. 106. Equipment for applying gaseous methyl bromide to nursery soils. Left, gas metered
from a cylinder, for large operations. Right, applicator for 1-lb. cans of gas for small operations.
T 202 1
Fig. 107. Diagrams showing the methods for stacking, covering, sealing, and injecting flats
of soil with gaseous methyl bromide.
Treating bulk soil
and ground beds
Bulk soil and ground beds may be
treated in the same way. Pile bulk soil
1 to 2 feet deep, be sure that it is not
excessively wet or cold, and treat as
shown in figure 107. For ground beds,
measure the area beneath the cover and
apply at 4 pounds per 100 square feet for
fungus control, or 1% to 2 pounds per
100 square feet for nematode and weed
control (fig. 125).
Effectiveness
Methyl bromide kills nematodes even
in unrotted galls, but it does not kill
V erticillium albo-atrum (which causes
wilt of chrysanthemum and numerous
other crops) and it may leave the soil
toxic for carnations. Consequently, it is
not recommended for carnations or
chrysanthemums. It is recommended for
bedding-plant operations where a rapid
turnover of soil and flats is required
and the short treatment period is neces-
sary.
The recommended dosage of 4 pounds
per 100 cubic feet will control all of the
common soil fungus diseases except
V erticillium wilt. Excellent weed con-
trol is obtained except for Malva and bur
clover. The user should not think treat-
ment unsuccessful if these weeds sur-
vive, but if many other weeds survive,
it indicates that the application was
faulty. Lower dosages have been suc-
cessfully used in warm sandy soils, and
growers have found that dosages as low
as 2 pounds per 100 cubic feet may be
effective.
Table 16 shows the approximate cost
of methyl bromide based upon the maxi-
mum dosage.
Formaldehyde
Formaldehyde is the chemical that has
been in longest use for soil fumigation,
and is still used as a drench for rooting
[203]
media and glasshouse benches. It is a
water-soluble liquid that penetrates
the soil as far as the water carrier and
volatilizes rapidly, one of the principal
advantages of this material. Since the
fumes are very toxic to near-by foliage,
it has restricted use in glasshouses with
living plants. It has been successfully
used in large glasshouses when the vents
were fully open and the treatment area
was somewhat removed from living
plants. Formaldehyde is very irritating
to eyes and nasal passages, and is ob-
noxious to use for this reason.
Commercial formaldehyde (37 to 40
per cent formaldehyde in water solu-
tion) at 1 pint in 61/4 gallons of water
is applied at the rate of % gallon per
square foot of soil surface. Soil is cov-
ered for 24 hours with plastic covers or
gas-resistant paper and then it is aerated
by thorough stirring.
The aeration period is from 10 to 14
days. The residual effects are very dam-
aging to seedlings and transplants and
care must be taken that all odor of the
gas is gone. A sure way to determine
whether soil is safely aerated is to plant
a few seedlings in it and see whether in-
jury results.
A dilute method has been prescribed
for damping-off control which may be
effective with lightly infested soils. It is
ineffective in heavily infested soil. By
this method 2 tablespoons (1 fl. oz.) of
formaldehyde in % cup (6 fl. oz.) of
water are sprinkled over a cubic foot of
moist soil which has been spread in a
thin layer; the soil is then mixed thor-
oughly, and stacked in clean flats and
covered with a tarpaulin or wet paper.
After 24 hours seeds may be sown, pro-
vided the flats are watered thoroughly
afterwards.
Vapam
Vapam, sodium N-methyl dithio-
carbamate dihydrate, has recently been
released for commercial use as a general
soil fumigant. It decomposes in soil to
form methyl isothiocyanate gas, which
is the active killing agent. It has been
successfully used to control weeds, nema-
todes, soil insects, and soil fungi, al-
though it is not recommended for eradi-
cative treatments. Since Vapam is solu-
ble in water, it may be applied by sprin-
kling or irrigating on the surface of the
soil or by injecting into soil with stand-
ard equipment. Consequently it is one
of the most versatile of the soil fumi-
gants. It has sufficient advantages to
warrant use, especially on crops grown
in the field or in ground beds. Although
Vapam may be used for treating flat or
potting soil, methyl bromide is usually
more satisfactory for these purposes.
Vapam is sold as a liquid containing
4 pounds of the active material per gal-
lon of water. Dosages are usually ex-
pressed as quarts or gallons of this for-
mulation to be applied to a given area
of soil. The dosage required depends
upon the organisms which are to be con-
trolled; for example, for weed control
it is from 1 to l1/^ pints per 100 square
feet and for fungus control it is from 1
to 2 quarts per 100 square feet.
Treating beds or benches
For small areas, such as ground beds
or benches, 1 quart of Vapam in 2 to 3
gallons of water in a sprinkling can may
be applied uniformly over the surface of
100 square feet of soil and immediately
followed with enough water to wet the
soil to a depth of 6 inches. This dosage
is approximately equivalent to 100 gal-
lons per acre, which is a good median
application for fungus control.
A hose proportioner may be used in
the same way with a stock solution of
1 quart of Vapam in 1 quart of water.
The proportioner ratio should not exceed
1:20.
Treating fields
For field applications either overhead
sprinklers or soil injectors may be used.
Overhead sprinkler applications may
[204]
be made by introducing Vapam into the
lines. The field is sprinkled for 5 to 10
minutes, then the required amount of
Vapam is introduced in the next 10 to 20
minutes. The sprinklers are then left on
until the soil is wet to a depth of 6 to 12
inches.
Vapam may be applied with stand-
ard knife-blade soil injectors set 6 inches
apart and 4 inches deep. The injection
method is useful because rows or strips
may be easily and inexpensively treated.
The row-treatment method has been
used with many field crops such as cot-
ton and beans, but surface applications
Lave been more widely used with orna-
mental crops.
As with all effective chemical soil
treatments, the soil should be in seedbed
condition at the time of treatment. Opti-
mum soil temperatures at the 4-inch
depth are from 55° to 65° F, although
Vapam has been successfully used at
temperatures of 45° to 70°. The tem-
peratures of California soils at planting
time do not ordinarily restrict its use,
although high temperatures may vola-
tilize the gas too rapidly, and surface ap-
plications should not be made on hot
days.
Seven days after treating, or when
soil has dried to a workable condition,
the soil should be cultivated lightly to
break the crust and facilitate aeration.
Usually treated soil may be planted 14
days after treatment unless prolonged
rains have prevented adequate aeration.
In such cases it is desirable to wait until
all odor of the gas is gone, or to make
test plantings before planting the main
crop.
Terraclor
Terraclor (PCNB), pentachloronitro-
benzene, has recently been marketed
as a soil fungicide. It differs from
most soil fungicides in its specificity of
action (for example, Rhizoctonia is con-
trolled, Pythium is not), its low toxicity
to many plants, and its relatively long
residual activity in soil. Another peculi-
arity of the compound is that it inhibits
growth of Rhizoctonia, but does not kill
it. Because of these factors it may be
used in several ways for disease control,
provided water molds are not present.
The compound is new and it must be
tried on many more ornamental plants
before it can be generally recommended.
The results on carnations obtained by
Sciaroni and Raabe (1955) and Scia-
roni (1955) are cited here as a guide for
use on other crops as well as for carna-
tions.
As a preplanting treatment the 75 per
cent wettable powder PCNB may be
dusted or sprayed on the soil surface at
the rate of 1 to 1% pounds per 1,000
square feet and mixed to a depth of 1 to
2 inches by raking. Carnation plants
may be set immediately in soil treated
in this manner without damage. Damp-
ing-off caused by Rhizoctonia has also
been effectively controlled in sweet-basil
plantings by application of the 75 per
cent wettable powder at 1 to 1% pounds
per 1,000 square feet immediately before
seeding. No seedling injury has been ob-
served.
In addition to the soil-surface method
of application, PCNB has been applied
as a strip treatment in the planting fur-
row at the time of planting. A general
recommendation for this method with
beans and cotton is to use 5 pounds of
the 75 per cent material in 10 gallons of
water per acre.
A unique use of PCNB has been its
application as a protective fungicide on
soil previously treated with steam or
chemicals such as chloropicrin, Vapam,
or methyl bromide. To protect against
infestation (sees. 3 and 14) of such
treated soil by Rhizoctonia, 1 to 1%
pounds PCNB (75 per cent wettable
powder) is applied to 1,000 square feet
of soil and raked into the top 1 to 2
inches just prior to planting.
[205]
NEMATOCIDES
Chloropicrin and methyl bromide eco-
nomically control nematodes in con-
tainer soils when other pathogens must
also be killed. For controlling nema-
todes alone in field soils, however, these
materials are too expensive. If nematodes
or soil insects are the problem one of
these nematocides may be used; but it
should not be used for control of damp-
ing-off or other fungus diseases. For
these reasons the recommendations
given for nematocides deal with field ap-
plications only. The same general soil
preparation as outlined for fungicides is
required for successful treatment for
nematodes.
Ethylene Dibromide
Ethylene dibromide is a liquid which
is applied to soil by a hand-injector or
by a continuous-flow applicator at the
rate of 3V2 to 7 gallons of actual ethylene
dibromide per acre. Since it is not so
volatile as chloropicrin or methyl bro-
mide, special covers or seals are not re-
quired for its use. This relatively low
volatility necessitates long aeration pe-
riods of 2 to 3 weeks before planting. It
should not be used on soil to be planted
to carnations.
D-D Mixture
D-D mixture (dichloropropane-dichlo-
ropropene) was the first of the cheap
effective nematocides. It is applied by
hand-injection or continuous-flow appli-
cators at the rate of 200 to 400 pounds
per acre. Planting must be delayed 1 to
2 weeks.
Nemagon and V-C 13
Nemagon (l,2-dibromo-3-chloropro-
pane) and V-C 13 (0-2,4-dichlorophenyl
0, 0-diethyl phosphorothioate) are newly
marketed nematocides which are said to
be nontoxic to many plants when applied
to soil around established root systems.
They represent promising developments
in nematode control, but cannot yet be
recommended for general use.
General Effectiveness of
Nematocides
These chemicals are very cheap and,
although nematodes are not completely
eradicated by treatment, sufficient con-
trol is obtainable to return the cost of
the treatment many times.
Many field-flower growers are now
using metering valves mounted above
the plowshares to drip soil fumigants
into the furrow during the plowing op-
eration. This practice fits in well with
the culture of most crops and has re-
duced the cost of nematode control,
since expensive injection machines are
not necessary.
INSECTICIDES
The common soil insects are all killed problem, two recently published pest-
by treatments which are effective against control guides (Jefferson and Pritchard,
fungi and nematodes, hence the specific 1956; Pritchard, 1949) may be con-
soil insecticides are not discussed here, suited for a description of the insecti-
In the event that insects are the main cides and treatments.
[206]
SOIL DRENCHES AROUND LIVING PLANTS
A few fungicides have been used as
soil drenches. These are applied to the
soil around the growing plant and are
used primarily to prevent enlargement
of an existing infestation. They are ma-
terials of limited volatility which kill by
direct contact with the parasites. They
are not recommended as primary dis-
ease-control materials, but they may be
useful in checking the spread of disease
that arises in a planting in spite of previ-
ous precautions. Soil drenches of this
type must penetrate the soil, kill or in-
hibit the fungus parasites, and be non-
toxic to the existing plants. Drenches
may suppress pathogens but do not eradi-
cate them, since none of the present ma-
terials are able to penetrate soils more
than a few inches. In addition, many of
them are rapidly inactivated in soil.
The most commonly used materials
for soil drenches are ferbam (Fermate),
Semesan, thiram (Arasan), captan
(Ortho 406), nabam (Dithane D-14),
and Terraclor (PCNB).
Terraclor (PCNB) may be used as a
soil drench for Rhizoctonia control on
living carnation plants at the rate of 1
to 1% pounds of the 75 per cent for-
mulation per 1,000 square feet. When
used in this way the obviously infected
plants should be removed and the chemi-
cal applied to an area extending 1 to 2
feet past the infested area.
Ferbam, thiram, and captan are usu-
ally applied at 1 tablespoon per gallon
of water at the rate of V2 to 1 pint per
square foot. Nabam may be diluted to
concentrations of 1:500 (V2 tablespoon
per gallon) and applied at the rate of
y<2. to 1 Pmt Per square foot.
Semesan at 1 tablespoon per gallon
of water is used at the rate of % Pmt per
square foot. Do not use Semesan on
roses in enclosed or poorly ventilated
areas since the mercury may volatilize
and cause severe injury. Semesan may
be effectively used against Rhizoctonia
damping-off on such plants as stocks,
but plants such as pansy, petunia, and
snapdragon may be stunted by its use.
Consequently, be careful in using Seme-
san if the tolerance of the crop to the
chemical is unknown.
In using drenches, remove all obvi-
ously diseased plants, drench the in-
fested area for 1 to 2 feet past the edges
of the infestation and repeat 7 to 10 days
later.
Since nabam penetrates deeper than
the solid materials, but has less residual
effect, a combination of it with one of
the other materials (for example, nabam,
y± tablespoon, plus captan, 1 tablespoon
per gallon of water) may be successful.
It must be remembered that these spot
treatments are not eradicative but tempo-
rary inhibitory treatments at best.li soil-
disease problems persist, they indicate
that some major contamination exists in
the operation of the nursery and efforts
should be made to see that soil, plants
and plant parts, and greenhouse are
made free of contaminating organisms
(sees. 8 through 13).
[207]
Table 17. Summary of Chemicals, Dosages, and Treatments Used to
Control Diseases and Nematodes in Nursery Soils
Chemical
Recommendations
SOIL FUMIGANTS— FUNGUS CONTROL
Chloropicrin
Formaldehyde
Methyl bromide
(gaseous)
Terraclor (PCNB)
Vapam
DOSAGE: Field: 3 cc per hole on 12-in. centers, 6 in. deep. Bulk
soil : 3-5 cc per cu. ft.
TREATMENT PERIOD: 1-3 days, confine with cover, wet news-
papers, or water seal.
AERATION: 7-10days or until all odor of gas is gone. Recommended
for carnation, chrysanthemum, field soil applications.
DOSAGE: As drench: 1 pint in 634 gal- water, applied at the rate
of Yz gal. per sq. ft.
TREATMENT PERIOD: 24 hr.
AERATION: 10-14 days. Stir thoroughly and do not plant until all
odor of chemical is gone.
DILUTE METHOD : 2 tbs. per % cup water. Sprinkle this amount
over each cu. ft. of moist soil spread in thin layer, stacked and
covered for 24 hr. Sow seeds after 24 hr. and water thoroughly.
Formaldehyde may be used as a drench for rooting beds and for
cleaning up greenhouse areas when plants are removed. Chloro-
picrin or methyl bromide is better suited for most nursery needs.
DOSAGE :41b. per 100 cu.ft.of bulk soil or 100 sq.ft. of soil surface.
TREATMENT PERIOD : 24-48 hr. Must be confined beneath gas-
proof cover.
AERATION : 24-48 hr. Very effective and especially suited for flat
and bulk soil fumigation. Do not use for carnations or chrysan-
themums.
DOSAGE: (for Rhizoctonia control) 1-1 y2 lb. (75% wettable pow-
der) per 1,000 sq. ft.
TREATMENT AND AERATION PERIOD : May plant immediately
after application.
DOSAGE: 1-2 qt. per 100 sq. ft.
TREATMENT AND AERATION PERIOD: 7-14 days. Longer
period required if soil is cold and wet after application.
GENERAL RECOMMENDATIONS : Use methyl bromide for soil in flats and containers,
chloropicrin or methyl bromide for bulk soils, and chloropicrin, methyl bromide, or
Vapam for other soils, whichever is most suited to your needs.
208 )
Table 17. (Concluded)
Chemical
Recommendations
SOIL FUMIGANTS— NEMATODE CONTROL
D-D mixture
Ethylene dibromide
Chloropicrin
Methyl bromide
(gaseous)
DOSAGE: 200-400 lb. per acre.
TREATMENT AND AERATION: 1-2 weeks.
DOSAGE: 3-6 gal. per acre for the 85% EDB. Dosage must be al-
tered according to the actual concentration of EDB in the material
used, since it is marketed in several forms.
TREATMENT AND AERATION: 2-3 weeks. Do not use for car-
nations.
This compound, when applied at dosages sufficient for fungus
disease control, will also kill nematodes. Other nematocides are
cheaper, however.
When used for fungus disease control, nematodes are also con-
trolled. It may be used at lower dosage for weed and nematode
control. More expensive than standard nematocides.
DOSAGE: 1^-2 lb. per 100 cu. ft. or sq. ft.
TREATMENT : 24-48 hr.
AERATION : 24-48 hr.
GENERAL RECOMMENDATIONS : If only nematode control is desired use D-D mix-
ture or ethylene dibromide, since they are cheaper and very effective. Do not use for
fungus control.
SOIL DRENCHES— SPOT TREATMENT FOR DAMPING-OFF CONTROL
Captan, ferbam,
thiram
Nabam
Semesan
Terraclor (PCNB)
Remove all diseased plants, drench area 1-2 ft. past the edges of
infestation and repeat 7-10 days later.
DOSAGE: 1 tb. per gal. water applied at the rate of M>-1 pint per
sq. ft.
Same as above except that dosage is M~3^ tb. per gal. Pene-
trates further than solid suspended materials in soil, but has less
residual effect.
Same as above except that dosage is 1 tb. per gal. water applied
at the rate of ^ pint per sq. ft. Since it contains mercury, do not
use near roses.
For Rhizoctonia control on carnation, remove all obviously infec-
ted plants, apply 1-13^2 lb. (75% wettable powder) per 1,000 sq.
ft. to an area extending 1-2 ft. beyond infected plants.
GENERAL RECOMMENDATIONS : All have been used with varying degrees of success.
These will not eradicate pathogens, but they may serve to check their advance.
[209]
SECTION
Treatment of
Nursery Containers
Kenneth F. Baker
Chester N. Roistacher
Philip A. Chandler
Heat treatment of containers
Chemical treatment of containers
.REATMENT OF NURSERY Soil to free it
of pathogenic organisms is rapidly be-
coming an accepted procedure in Cali-
fornia. Such disinfestation, either by
steam or chemicals, is best performed in
the containers (for example, flats, pots,
cans, or benches) in which the soil is to
be used. There are some situations in
which this is impracticable, however, and
soil is treated in bulk (sees. 8 through
11) . There must then be some additional
means of treating the containers if dis-
ease control is to be achieved. Placing
treated soil in infested containers per-
mits rapid extension of pathogens and
usually leads to severe disease losses
(sees. 3 and 14). On the other hand, if
containers are treated, bulk soil may be
steamed and placed in them with no
greater disease hazard than the possi-
bility of contamination from handling.
Since such an operation is commercially
feasible, methods for container treat-
ment are presented in this section.
HEAT TREATMENT OF CONTAINERS
Heat treatment of containers is not ap-
preciably different from the steaming of
soil discussed in Section 8, either in
methods or temperatures required. After
CAUTION:
Many
of
the chemicals
mentioned
in this
manual are
poi-
sonous anc
may
be
harmful.
The
user should
carefu
lly
Follow the
pre-
cautions on
the 1
□ be
Is of the
con-
tainers.
steaming, flats or pots may be filled with
treated soil and planted immediately,
whereas those chemically treated require
a period of aeration before use. Steam
may also be used without injury to near-
by living plants or irritation to workers,
in contrast to most chemicals, which
cannot safely be used in confined areas.
Containers may be placed in a bench and
covered with a tarpaulin beneath which
steam is released. Equipment used for
treating soil in containers (Sec. 10) may
also be used for this purpose.
[210]
Flats
The minimum treatment should be at
least 180° F for 30 minutes, and there
is no harm from higher steam tempera-
tures. Flats may be steamed in stacks
either covered with heavy tarpaulins, or
placed in a chamber with flowing steam
or in a pressure container (Sec. 10).
Flats should be separated from each
other horizontally by %-inch strips, or
stacked in a staggered manner with ver-
tical spaces of about 1 inch (fig. 104).
This will permit the free flow of steam,
and make for faster, more economical
heating. This process can be mechanized
by stacking flats on pallets for handling
by fork-lift tractors (Sec. 17) ; such a
practice would decrease the chance of
recontamination by keeping treated flats
off the ground and by reducing han-
dling. In any case, the pallets should be
treated before re-use.
Continuous steam tunnels have been
used in canneries and fruit packing-
houses for sterilizing of lug boxes be-
fore re-use. In general, it has been found
that exposure of 2 minutes to flowing
steam of 212° F is necessary to destroy
molds in corners of the boxes. Results
with nursery flats should be comparable.
The time might be shortened somewhat
by using superheated steam. From the
standpoints of efficient use of steam and
avoiding moving parts, the use of space
steaming in piles described above is to
be preferred.
Benches
Benches are satisfactorily treated by
steaming them under a tarpaulin. As
with flats, the minimum treatment should
be 180° F for 30 minutes.
It should be pointed out that the use
of intense localized heat on benches,
flats, and so on, may not be satisfactory.
Sometimes nurserymen rapidly go over
their benches with a blowtorch. This
practice is of little use because it would
be necessary to char the surface in order
to heat in the cracks.
Somewhat better is the use of a jet of
flowing steam directed on the surface; if
continued long enough to heat the ma-
terial it is satisfactory. So much steam
is lost in this method, however, that it is
prohibitively expensive. By confining
the steam, one obtains the efficient space
treatment described above.
Clay pots
Empty clay pots present a special
problem in California nurseries. Water
is continually evaporating from the
porous surface and leaving a deposit of
soluble salts that in time becomes clearly
visible (Sec. 4). In most nursery soils
the roots tend to grow out to the pot and
then to spiral, forming a more or less
hollow cone. Most of the roots are then
located in the highly saline zone, with
resultant stunting of plant growth.
There are three ways of reducing this
hazard:
1. Using a nonporous container (for
example, cans, plastic pots, or painting
the inside of clay pots) as discussed in
Section 4. The success of this method is
shown by the common use of cans in
California nurseries.
2. Using a light porous soil mix of the
U. C. type. This provides favorable aera-
tion conditions for roots throughout the
soil mass instead of just at the sides, as
occurs with heavy soils (fig. 61). Such
a low-salinity, well-aerated soil there-
fore reduces the seriousness of salt ac-
cumulation in clay pots, but cannot
eliminate it.
3. Soaking of clay pots for 24 hours
or more in water, then washing them in
the usual way. We have found that this
practice has largely solved the salt prob-
lem. It is possible, therefore, to achieve
a reduction of salinity and to disinfest
the pots in one operation by heating the
water in which they are soaked to 140°
to 180° F. This will destroy the algae
and mosses, as well as disease organisms
that commonly persist from one plant-
[211]
ing to the next. The pots may then be
washed if desired.
It is considered that hot-water treat-
ment of clay pots is preferable to steam-
ing in California, because of the salinity
problem. If, however, the empty pots are
not soaked, they definitely should be
steamed before re-use, heating to 180° F
for 30 minutes. They can be efficiently
handled when nested in horizontal rows,
and may be handled on a pallet equipped
with sideposts (fig. 134).
Metal or plastic containers
Metal or plastic containers that are so
tapered that they nest may be steamed
but must be stacked vertically; it is un-
necessary to soak them, however.
CHEMICAL TREATMENTS OF CONTAINERS
Containers disinfested with some
chemicals must be aerated to dispel the
materials before use. With some ma-
terials (for example, methyl bromide
and copper naphthenate) the delay is
short and reasonably convenient, but
with others (for example, formaldehyde)
it may last for several days. Some of
these materials are harmful to plants and
annoying to workmen, and must be han-
dled accordingly.
Copper naphthenate is retained by
wood for a year or more and thus pro-
vides a self-disinfesting surface.
Methyl Bromide
Methyl bromide is used at the same
dosage, 4 pounds per 100 cubic feet of
space, and in the same way as for soil
(Sec. 11). Containers should be aerated
for 1 day before use. This is a very satis-
factory method for the nursery with
types of steaming equipment that make
no provision for container treatment. It
is of limited value to a nursery that uses
chemicals for soil treatment, since the
soil should in such cases be treated after
being placed in the container. Methyl
bromide is expensive to use for empty
flats or pots because the dosage is the
same as if they were filled with soil; see
Section 1 1 for approximate costs. This
material effectively disinfests the flats or
pots, but, unlike copper naphthenate,
leaves no residue that will reduce recon-
tamination.
In New York it has been found (Lear
and Mai, 1952) that methyl bromide at
4.6 pounds per 100 cubic feet of space
may be used to treat bales of burlap
bags, farm machinery, and other equip-
ment to free them of nematodes. Trucks
were covered with polyethylene tarps
and treated without sustaining damage.
It is desirable first to wash dried mud
from under fenders and wherever it has
accumulated.
Formaldehyde
Formaldehyde is an excellent fungi-
cide, although an obnoxious one and
therefore not frequently used for con-
tainer treatment. It is used at a dilution
of 1 gallon of commercial formaldehyde
(37 per cent concentration) to 18 gal-
lons of water. Application is made by
dipping or spraying flats, pots, or other
containers. They may be immersed for a
few minutes in the material, permitted
to stand until the excess has drained
back into the tank, then stacked. For-
maldehyde in the above concentration
may be sprayed on containers until they
are thoroughly wetted, using a very
coarse nozzle to minimize volatilization.
In either case the containers should be
stacked while still wet, and preferably
covered with a tarp for 24 hours. When
they are uncovered they should not be
permitted to become dry at any time
until the odor of formaldehyde is gone
(usually less than 5 days). The water in
[212]
a formaldehyde solution will evaporate
before the formaldehyde volatilizes, and
the chemical then passes over to a white
powder, paraformaldehyde. From this
state it volatilizes at a much slower rate
than from a water solution. For example,
flats kept wet were free of formaldehyde
in 4 to 5 days, whereas those permitted
to dry were found to require 10 days to
reach comparable levels. It should be
noted that the rate of volatilization from
paraformaldehyde may be so low as not
to be detected, but that if the flats are
again wetted it may appear in amounts
toxic to plants.
It is a wise precaution to check care-
fully for the presence of formaldehyde
before planting flats. To do this, wrap
moist sample flats in a piece of poly-
ethylene plastic for 24 hours, then open
one side to see whether the odor of the
fumes can be detected. An even safer
method is to fill several flats with soil,
plant sensitive seedlings (for example,
petunia) in them, then cover with a poly-
ethylene tarp for 24 hours. Injury will
be evident on seedlings near the sides
of the flat within 2 days as white dead
areas in the leaves.
The highly irritating nature of for-
maldehyde fumes makes indoor use ob-
jectionable. It should never be used in
the same room with living plants. Con-
tainers are best treated and aired out-
doors, down-wind from the growing
areas. Workers should remain up-wind
from the material, and in still weather a
fan might be used. They should wear
rubber gloves when handling the treated
flats, and tight goggles when spraying
the chemical on flats. Use of a full-face
gas mask may be desirable.
Formaldehyde is extremely useful as
a rapid disinfestant for tools (Sec. 3).
If it is used on benches, lath shade-
frames, or glasshouses, the same pre-
cautions regarding application, keeping
wet, and aeration should be observed to
prevent injury to plants or workers.
It should be noted that formaldehyde,
like methyl bromide, leaves no perma-
nent residue that will reduce recontami-
nation.
Formaldehyde-steam
A southern California mushroom
grower has successfully used formalde-
hyde-steam mixtures (Sec. 10, type 26)
for disinfesting his houses. This tech-
nique is worthy of trial for treating
glasshouses between crops.
Copper Naphthenate
Methods of application
Copper naphthenate is an excellent
material for treatment of wooden con-
tainers. It prevents fungi from growing
on or into wood which it thus protects
from decay, as well as rendering the con-
tainers self-disinfesting for a time. It is
available in bulk as a concentrate having
8 per cent copper (see Appendix) that
may be diluted with Stoddard solvent (1
gal. of the napthenate to 3 gal. of sol-
vent) to a concentration of 2 per cent
copper. This is applied by dipping for
5 to 30 minutes either the finished flats
or the shook for making them, in a tank
of the chemical. The excess is drained
back into the tank, and the containers
then aerated for a day. The material may
also be brushed on. A gallon of material
covers from 200 to 400 square feet of
surface by either method of application,
according to the smoothness of the wood
treated. Diluted copper naphthenate sold
under several trade names may be much
more expensive than the above but
equally satisfactory.
The corrosive effect of treated wood
on iron or galvanized nails has been
eliminated by using aluminum nails in
constructing flats, benches, and so on.
Effectiveness
Of the materials presently available,
copper napthenate most nearly fulfills
[213]
B
\v
Mi Mat •* ;•
[214]
the requirements of a residual flat disin-
festant. It kills pathogens near or in
contact with the wood by slowly leaching
into the soil for a distance of 1 to 2
inches from the wood. Although it is
injurious to roots that enter this zone,
for many nursery purposes it is reason-
ably satisfactory. It is still effective after
a year's contact with moist soil. That it
is relatively inexpensive is shown by the
fact that nurserymen have found it
economically justified even when used
solely as a wood protective.
In repeated tests, treated flats have Dot
carried damping-off fungi from a plant-
ing of infested soil to a subsequent one
of steamed soil 'fig. 108, A I . even
though emptied and refilled six times.
The flats should be rinsed lightly with
water before re-using, in order to re-
move the attached soil.
Injury to seedlings
Injury to roots that enter the zone
usually is seen as darkening, or even
killing of the tips i fig. 108. B i . Such in-
jury occurred on seedling roots of all
plants tested, but some of them I pepper.
pea. nasturtium, calendula ' show no
corresponding injury to top growth.
Others | tobacco, larkspur. Iceland
poppy, snapdragon, petunia, pansy. Lo-
belia. Coreopsis. }<emesia. China aster,
and stock > show varying degrees of in-
jury around the edges of the flats i fig.
108. C).
It is apparent that copper napthenate
is somewhat more soluble than necessary
to achieve the self-disinfesting properly;
on the other hand. Wolman salts and
Erdalith • see below i are too insoluble.
Perhaps an intermediate level of solubil-
ity mav later be achieved that will be
self-disinfesting but less injurious to
roots. Tests have shown that the Stod-
dard solvent is not the source of residual
toxicity, for it volatilizes rapidly.
Uses
It should be emphasized that many
growers are unaware of the injurious
effect of this material, and that it should
be decided in each instance whether its
usefulness exceeds its injuriousness. As
a suggestion, the following uses may be
cited.
Copper naphthenate may safely be
used on benches and shelves on which
flats or other containers are to be placed.
It is excellent for treating timbers to
be placed on the ground for supporting
flats I Sec. 3 I .
It is verv useful for disinfecting a
glasshouse bench before filling it with
soil, under conditions where living
plants must remain in the house. If the
ventilators are kept open until the Stod-
dard solvent has evaporated 1 12 to 24
hours | there is little danger to surround-
ing plants. It should be noted that some
sensitive plants, such as maidenhair
fern, may be injured by the volatile sol-
vent under conditions of inadequate
ventilation. The copper naphthenate resi-
due is not volatile and does not injure
adjacent plants.
The chemical mav safely be used on
flats or benches which are to be filled
with soil and used for large plants, or in
which seedlings are planted 2 to 3 inches
from the sides.
It should not be used on seed flats or
on containers in experimental work.
Apparently it is toxic to large geraniums
Fig. 108. Effect of copper-naphthenate treatment of flats on carryover of damping-off fungi,
and on seedlings grown in them. Untreated flats at left, treated at right in each case. Steamed
soil used in all cases. A, Effect on carryover of R" zcc^cr'a on a flat from a previous diseased
planting, as shown by damping-off of pepper seedlings. Note elimination of marginal damping-
off by t-eatment. B, injury to pepper root tips from a flat planted with four changes of soil in
4 months since treatment. C, Toxicity to tobacco seedlings from a flat treated and aerated for
10 days before seeding; half flats are shown.
[ 215 ]
grown in clay pots treated with it, and
its use on such containers is inadvisable.
Other Materials
Several chemicals have been used at
one time or another for container treat-
ment, without general adoption. Among
these are the following.
Ethylene oxide gas (Carboxide:
contains 10 per cent ethylene oxide in
90 per cent carbon dioxide) used at 0.5
pound of active ingredient per 100
cubic feet has been effective in destroy-
ing the bacteria that cause potato ring
rot in 16 hours in fumigation chambers.
It has also been used for soil at some-
what higher dosages.
Sodium hypochlorite solutions
have been successfully used for disin-
festation of bulb trays, fruit boxes, and
similar equipment. Commercial solu-
tions (for example, Clorox, Purex)
usually have about 5 per cent available
chlorine, and are diluted to 0.4 per cent
(1 quart to 3% gallons) or 0.2 per cent
(1 quart to 61/4 gallons) . They are either
used as dips or sprayed on the containers,
and may be covered with a polyethylene
tarpaulin for 24 hours.
Fixed wood preservatives such as
Wolman salts, Erdalith, and Celcure are
so firmly stabilized in the wood as to be
valueless in producing self-disinfesting
flats. They are, however, excellent wood
preservatives and are not generally
harmful to plant roots.
[216]
SECTION
Development and
Maintenance of Healthy
Planting Stock
Kenneth F. Baker
Philip A. Chandler
Importance of clean propagating material
How to obtain clean seed or stock
Maintaining clean stock
I
T has already been pointed out I See.
3 i that plant-disease organisms may get
into a planting from I 1 | the soil. I 2 I
the seeds, cuttings, bulbs, or other
propagative stock, or 1 3 1 from con-
taminated containers or tools, or from
infected material splashed, blown, or
otherwise dispersed. Soil infestation is
discussed in sections 3. 14. and 15, and
methods for controlling it in sections 3
and 8 through 11. The recontamination
problem and its control are considered
in sections 1, 3. 12. and 14. There re-
mains the propagative material to be
discussed in this section, explaining how
such stock may be produced and used,
and the benefits to be derived from us-
ing it.
Almost anyone associated with the
nursery business will agree that patho-
gen-free planting stock is desirable.
There may be differences of opinion on
methods for producing such material,
the price one can justifiably pav for it.
and the best ways to use it in commercial
growing. The proper use of clean seed
and stock probably will be profitable
anytime, and might prevent bankruptcy.
That we fall far short of the ideal in
production and utilization of such stock
is shown bv the rapid increase in fungi-
cide sales to nurseries in recent years.
Two types of nurservmen are inter-
ested in pathogen-free planting stock:
(1) one who produces plants or flowers
for market. He wishes clean stock as a
means toward an end, the cheapest, most
dependable possible production of
plants, \\hen possible, clean stock should
be obtained by such a nurseryman from
a specialist propagator. L nf ortunatelv.
pathogen-free stock of onlv a few crops
is presently available, and the grower
must usually develop his own supply
along the lines discussed here. This sec-
tion is presented primarily to assist such
a grower. As he begins to provide clean
stock to others he often gradually be-
[217]
comes a (2) specialist propagator, to cultural operation, most of which must
whom the production of pathogen-free be locally evolved as needed. Therefore,
stock is the end desired. This business it is expected that this section will be
involves much highly specific informa- less useful at the specialist level than for
tion for the given crop, disease, and the general grower.
IMPORTANCE OF CLEAN PROPAGATING MATERIAL
Only a small percentage of seed or
propagative stock ordinarily is infested,
but this is of the greatest importance
because it serves as a center of infection.
Whether the pathogen spreads with soil,
as in the case of most of the fungi con-
sidered in this manual, or by spores, the
end result is to start a series of "spot
ires.
Rapid increase of pathogens
Other conditions being equal, the
greater the number of spores produced
by a fungus, or eggs by a nematode, the
more effective and rapid is its spread.
Although the dissemination process is
prodigiously wasteful, its effectiveness
cannot be doubted. From a single sclero-
tium of the cottony-rot fungus (Sclero-
tinia sclerotiorum) are produced several
tiny, cup-shaped structures said to form
as many as 310,000,000 spores. A single
leaf spot of celery Septoria late blight
may produce more than 200,000 spores.
A single female root-knot nematode com-
monly lays 500 to 1,000 eggs and may
even reach 2,800; a single gall may con-
tain many such adults. Snapdragon rust
has been conservatively estimated to be
able to increase from a single rust pus-
tule in a shipment of 10,000 plants to
an average of 4,600 lesions on each plant
90 days later. The grower who believes
that diseases "suddenly appear" is ob-
serving only the final stages in their
build-up. Because of such rapid increase
it is particularly important that initial
infections be prevented. Epidemics, like
fires, are best stopped while they are
small.
Importance of
initial infections
The relative importance of each infec-
tion is determined by its newness in that
location, and by its permanence. The
ascending progression of danger may be
given as follows:
1. Least important are those organ-
isms that are already present in the area
and do not infest soil (for example,
snapdragon rust in California). The
centers of disease serve as temporary
foci of infection and may be controlled
or reduced in severity by fungicidal
treatment.
2. Somewhat more serious are organ-
isms already present in an area and able
to infest soil. If the organism infests the
land for only a few years, as with Alter -
naria disease of zinnia, bacterial blight
of stock, and bacterial stem rot of del-
phinium, it is bad enough.
3. If, however, the pathogen is present
and remains permanently in the soil, as
with Fusarium wilt of aster, Phytoph-
thora root rot of heather, and Rhizoc-
tonia diseases, it is a serious matter.
4. Those organisms introduced to new
areas but not infesting soil (for example,
the appearance in 1952 of snapdragon
rust in Australia) may create much ex-
citement and become very important.
5. A still worse situation is the intro-
duction to a new area of an organism
that will persist in the soil. As in 2 above,
this is serious if the organism infests
soil only temporarily (for example, mov-
ing crown-gall infected cuttings into
virgin land) .
[218]
6. When the new pathogen perma-
nently infests the land, as with the intro-
duction of Phytophthora cinnamomi on
young heather plants from southern to
central California, the worst situation of
all is reached.
The organisms discussed in this
manual fall into categories 3 and 6, de-
pending on whether or not they are new
to an area. Since not all types of a given
fungus are identical in response to either
environment or host plants (Sec. 15),
we are here concerned almost entirely
with category 6, the worst of all.
Benefits from use
The practical benefits from using
clean propagating stock are essentially
those outlined for the complete disease-
control program (sees. 1, 2, 3, 16, and
17). Among these benefits are reducing
production cost and possibly reducing
competition, as well as aiding easier,
more certain, less expensive production.
HOW TO OBTAIN CLEAN SEED OR STOCK
The first step in a program of this sort
is to obtain the initial healthy seed or
stock. In some cases (for example, seed
of garden stock; chrysanthemum cut-
tings) these can be purchased from a
specialist grower who maintains them.
In most instances, however, the nursery-
man must still develop his own clean
stock. The methods used in either case
are outlined here, with details of the
second types. Since recommendations
could not be given for each of the many
nursery crops, even if they had b:en
studied, the various methods are pre-
sented, with applications indicated for
some specific plants.
Man's experience with his own fal-
libility has often caused him to provide
more than a single defense against ad-
versity, as insurance companies are
aware. This also applies to disease con-
trol. Thus, a grower may discard all
obviously diseased stock, treat the re-
mainder, avoid overhead sprinkling or
other cultural practice that favors the
pathogen, remove any diseased plants
that appear in order to reduce inoculum,
and spray regularly to protect against
any spores that blow in. Rarely is a
single control measure sufficient to pre-
vent a plant disease. This is true of the
nursery diseases discussed in this
manual, and particularly so in the de-
velopment and production of pathogen-
free stock. Hence several concurrent
procedures are often suggested to
achieve this objective.
If a few healthy plants can be found,
the grower can propagate from these by
observing reasonable sanitary proce-
dures (Sec. 1). These often cannot be
found, however, and the grower must
resort to other more involved techniques.
Plant Grows away from the
Pathogen
It is possible in some cases, by mani-
pulation of the environment or cultural
practices, to obtain clean stock from
diseased plants. The plant may be grown
in such a way that the propagative parts
remain uninfected because they develop
in a position and under conditions un-
favorable to the disease.
Tip cuttings
Thus, it is possible to reduce (but not
commercially to eliminate) V erticillium
wilt from chrysanthemum by taking tip
cuttings from rapidly growing shoots at
least 12 inches above the ground. If each
cutting is then established in a separate
pot of steamed soil, grown to maturity,
only healthy plants used in propagation,
and the process repeated, it should be
possible to derive clean stock. It is now
[219]
done faster and more reliably by "Cul-
turing Methods" (see below). With
fungi (for example, Rhizoctonia and
water molds) that do not invade the
water-conducting system (as do Verti-
cillium and Fusarium) this is more
easily accomplished.
It is possible1 to get Choisya cuttings
free from Phytophthora by taking them
from large shrubs at a point at least 4
feet from the ground, and by rooting and
growing them in steamed media to pro-
duce gallon-can stock without disease
loss. This is in striking contrast to the
50 to 90 per cent mortality in many nurs-
eries. Furthermore, these plants have
grown exceptionally well when planted
in gardens. It is, of course, necessary
that such cuttings be taken in the dry
season, that the shrubs either not be
splashed with mud or debris by rains,
down-spouts, sprinklers, or other ways,
or that the shrubs be so high that such
spattering does not occur at the levels
where cuttings are taken. It is further
necessary that cuttings be placed
on clean papers or in steamed baskets,
never on the ground, to avoid con-
taminating them. Cuttings should not be
taken, unless it is absolutely imperative
to do so, from known infected plants or
infested areas. These same conditions
apply equally to all other types of plant-
ing material discussed herein.
Similarly, the taking of azalea and
camellia cuttings from high shrubs
rather than low plants 6 to 12 inches
from the ground, as is so often done,
would greatly reduce carryover of
Rhizoctonia and water molds. A similar
method has been used in Oregon to ob-
tain strawberry plants free of the Phy-
tophthora that causes red stele.
The same method would free heather
cuttings of Rhizoctonia and of Phytoph-
1 Demonstrated in 1954 by J. A. Bcutel (As-
Bistanl Agriculturist, Farm Advisor's Office, Los
Angeles County) in tin- Department of Plant
Pathology, University of California, Los An-
geles.
thora cinnamomi, cause of one of the
principal diseases of the crop.
Application of this general system
could also provide a source of planting
stocks free from root-knot nematode and
the oak-root fungus.
By such careful manipulations, and
strict avoidance of overhead watering,
syringing, or spraying, it should be pos-
sible to obtain cuttings of marguerite
daisies, shrubs, and other plants, free of
crown gall, and oleanders free of stem
and leaf gall.
Araucaria tip cuttings taken from
plants grown to a height of 4 to 5 feet
under conditions free from splashing,
would be uncontaminated by Rhizoc-
tonia.
It is worth an attempt to develop a
nucleus stock of Esther Read daisy free
of bacterial fasciation by (1) training
up the shoots, (2) scrupulously avoiding
sprinkling, syringing, or spraying of the
plants, (3) taking tip cuttings, and (4)
rooting and growing them in individual
pots free from all water splashing.
Plants on frames
A modification of this is to train cane-
forming plants, such as Dieffenbachia
and some Philodendrons, so that the tips
are taken several feet above the ground.
This will free them of Rhizoctonia and
water molds, and if overhead watering
and high humidity are avoided, will
eliminate bacterial soft rot as well.
Peperomia may easily be freed from
Rhizoctonia and water molds by taking
tip cuttings from high on the plant. We
easily freed fuchsia and coleus plants
from foliar nematode by growing them
in a glasshouse without wetting the
foliage, even when the diseased leaves
were not removed, as they should have
been. Tip cuttings taken from these
plants* 6 to 12 inches above infected
leaves remained healthy.
By growing on wooden or wire up-
rights or frames to get the plants as far
off the soil as possible, and avoiding all
[220]
splashing water, it is easy to free such
trailing plants as Pellionia, Fittonia,
Nephthytis, Philodendron cordatum,
and ivy from Rhizoctonia and water
molds. Similarly, ivy may also be freed
of bacterial leaf spot. It would seem a
reasonable precaution to continue to
raise all mother stocks of these plants
in this way.
Aseptic culturing
of growing point
A further refinement is to make tiny
cuttings of the growing tip, to graft the
tips onto healthy plants, or to aseptically
culture the tiny apical growing point
(much as plant breeders culture em-
bryos) in order to free the plant of
viruses. Holmes (1955, 1956a, 19566)
and Martin (1954) have thus freed
dahlia of the spotted-wilt virus, chrysan-
themum of the aspermy virus, and sweet
potato of another virus. Norris (1954)
also eliminated virus X from potato in
this way. The technique might well be
extended to other kinds of plants by a
trained specialist. It is based on the
fact that some viruses, under certain en-
vironmental conditions, move slowly
through tissue and may not reach the
growing point. Quak (1957) freed car-
nations of viruses by culturing apical
meristems grown under high tempera-
tures.
Environmental control
In these techniques it is desirable to
make the environment as unfavorable as
possible for the pathogen without unduly
checking the growth of the host. Rhizoc-
tonia and water molds, under moderately
dry conditions, are unable to spread
much above the soil surface. Tempera-
ture control might increase this differen-
tiation between pathogen and plant.
Culturing Methods
This method apparently was first sug-
gested by A. W. Dimock of Cornell Uni-
versity in 1943 against V erticillium wilt
of chrysanthemum, and was soon
adopted by a commercial propagator.
In 1949 nearly 26!/2 million mum cut-
tings were produced in Ohio, 69.5 per
cent of the national total, largely by this
concern. This technique is best per-
formed by the specialist, although it is
now used by a number of growers in
various parts of the country. It has also
been adapted for use in securing Verti-
cillium-iree sticks of rose budwood by
Wilhelm and Raabe (1956), pathogen-
free carnation stock by Tammen, Baker,
and Holley (1956), and pathogen-free
geranium stock by Munnecke (1956).
It will undoubtedly be found useful for
many other crops grown in nurseries.
Although it is best adapted to use
against pathogens of either the systemic
or vascular type, it can be used on a
wide variety of plants and diseases.
As is often the case, the method is
basically simple, but becomes complex
from the number of unusual circum-
stances that may arise. Briefly, the
method (fig. 109) is as follows: Each
4-inch cutting (fig. 109, A) and a cor-
responding tube of nutrient agar are
assigned a number. A 1-inch piece (B)
is cut from the base of the cutting and
immersed in a Clorox solution (1 volume
to 4 of water) for at least 1 minute (C) .
The scalpel is flamed between cuts. The
piece is placed on a paper towel to drain
(D) for a few minutes, and the basal
!/4 inch is removed. Four slices each
y%2 inch thick are then cut off and re-
tained; the remaining ends are dis-
carded. The stem is cut on the paper towel
with a flamed scalpel. The four thin slices
are transferred to a numbered agar slant
(or tube of broth, if bacteria are in-
volved) and held at 75° to 80° F (E) .
The cuttings are then held in polyethy-
lene bags in cold storage, or planted in
paper cups of moist sterile media (F) for
10 days or more until readings are taken
on the tubes. If any of the four pieces in
a tube show any fungus or bacterial
growth, the corresponding cutting is de-
[221]
^9
"73
Fig. 109. Culturing method for selecting chrysanthemum cuttings free of Verticillium. See p.
221 and 222 for explanation.
stroyed. The remaining healthy cuttings have infested the soil and infected neigh-
(G), when rooted and grown on, become boring plants.
the nucleus block. The cuttings produced Modifications of this culturing process
by this block are grown in an increase have been introduced. Plain agar plus
block, from which cuttings are marketed
without additional culturing.
The principle is to determine rapidly
whether any fungus or bacterium is
present thai might not normally be de-
ter led until later, when it would already
sterile, dried, chopped plant tissue may
be used instead of nutrient agar when
bacteria are not involved. This is par-
ticularly useful for detecting Verticil-
lium. Petri dishes, rather than tube
slants, are then used.
222 |
Heat Treatment of Planting Stock
This method, introduced more than
70 years ago in Denmark, has, except
for cereal seeds, only recently come into
commercial application. Its effectiveness
is based on the principle that some or-
ganisms are more easily killed by heat
than is the crop plant. Heat has been ap-
plied through the agency of water, dry
air, moist air, and carbon tetrachloride.
At present, water is the best for rapid
treatments since its heat conductivity is
more than twenty times that of dry air.
The use of carbon tetrachloride is still
experimental. For long treatments (for
example, with some virus diseases), ex-
posure to moist or dry air is most useful.
Neither all kinds of plants nor all their
parts (for example, seeds vs. leaves) are
equally heat-susceptible, nor are all types
of growth (for example, lush succulent
tops vs. hard woody stems). The "trick"
for successful treatment often lies in se-
lecting the most heat-tolerant host tissue,
and manipulating culture procedures so
as to produce the most resistant growth.
Failure to consider these basic facts has
led to many "successful operations"
from which the patients did not recover.
injury may be avoided
Plant injury from heat treatment
ranges from induced dormancy of vege-
tative parts (for example, gladiolus cor-
mels), through delayed seed germina-
tion, production of weak and deformed
seedlings, to killing of some or all of
the material treated (reduced stand).
Injury may be reduced by using seed
relatively free from mechanical breakage
of the coat, and by avoiding seed over
2 years old. Nurserymen frequently
overlook the fact that seed or propaga-
tive material is one of their smallest
expenses, and that increased rate of
seeding will adjust for germination loss.
It often would be better to heat-treat the
stock and eliminate disease, even though
it reduced the germination 50 per cent,
than to plant it untreated and risk 100
per cent loss from disease. For a specialist
propagator the economic limits of treat-
ment injury are much higher; in many
cases the survival of only a single plant
from a given lot is justified if it provides
the start for a healthy mother block.
Heat treatment has limited direct use in
retail production, but it is becoming an
invaluable tool in propagative activities.
Value of treatment
Since heat treatment is eradicative,
aiming at elimination of the organism
from the tissue, it is used primarily for
situations where the pathogen is internal
and not, therefore, reached by external
chemical treatments. Heat is effective,
however, against spores and mycelium
both on the surface and borne internally.
The principal value of heat treatment lies
in preventing contamination of the soil
and the surrounding plants when set in
the field. It does not, however, provide
any protection of the plant against sub-
sequent fungi to which it may be ex-
posed. There is no reason from a disease
standpoint, therefore, to heat-treat seed
known to be free of pathogens.
There are several stages in a treatment
program; not all of these necessarily
apply to each type of material.
Selecting material to treat
Select for treatment the cleanest seed,
plants, or bulbs available. This would
also include selecting fresh seed, rather
than that several years old. In general,
only the cleanest and most vigorous
stock available is worth the effort the
treatment requires. Heat treatment is a
method for obtaining clean stock, not a
means of utilizing low-grade or worth-
less planting material!
Conditioning the material
Get the material into the best possible
condition for treatment. With many
foliage plants this may require growing
them, if in soil, for 3 to 6 months with-
out nitrogen fertilization and only
[223]
enough water to prevent wilting. A faster
system might be to wash the soil from
the roots and set the plants in fairly
coarse sand in order to reduce both
nitrogen and water intake. Humidifiers
and shading should be used only as
necessary to prevent burning. Neph-
thytis, Dieffenbachia, Fittonia, and Pel-
lionia benefit greatly from hardening
prior to treatment. Such hardening of
stock should be practiced before treat-
ing to obtain the original pathogen-free
material with which to establish a
mother block. Further propagation
should, of course, be from the un-
hardened mother block, since the com-
plete procedure is too costly and slow for
general propagation.
It has been found that gladiolus cor-
mels produced in warm, relatively dry
California soils are more tolerant of heat
treatment than are those grown in
cooler moister areas.
Calla rhizomes will tolerate 122° F
for 3 hours2 when in the desiccated
market condition, whereas freshly dug,
actively growing rhizomes and fleshy
stems may be killed in a half hour.
Preparing the material
for treatment
Preparation for treatment involves
trimming of dead leaves, roots, and
other parts, washing to remove dirt, and
any necessary dividing of clumps. No
more wounds should be made than ab-
solutely necessary, as water-soaking
occurs at such points. Dieffenbachia
cane is left in pieces up to 2 feet long,
and is divided to single-bud pieces
several weeks after treatment. In our
experience plant material is not success-
fully freed of a pathogen if left in the
soil-ball or pot. The cooling effect of the
soil and pot on the water, and the slow
penetration of heat into the soil, prevent
real effectiveness. Plants should always
he liare-rooted for treatment.
I apublished data of S. Wilhelm, obtained
in the Departmenl of Plant Pathology, Univer-
-iiv nf California, Loa Angeles.
Presoaking
A presoak is desirable in cool water
for 4 to 12 hours (nasturtium seed) to
displace air between layers, or for 48
hours in warm water (gladiolus cor-
mels) to displace air and render fungus
mycelium more susceptible. The use of a
presoak should be considered whenever
plant parts have loose coverings that trap
air and cause material to float.
Treatment equipment
and temperature
Heat treatment on a large scale is best
performed in a tank holding at least 100
to 200 gallons of water, because the
temperature is much more stable with
such volume. Equipment of this type is
commercially available as bulb-treat-
ment tanks (fig. 110; see also Appen-
dix), and one unit combines facilities
for steaming soil and treating plant ma-
terial (Sec. 10, type 7). Heat may be
supplied by a small stream of water from
a tap 20 to 30 degrees F higher than the
treatment temperature; this can usually
be achieved by turning up the thermo-
stat on the water heater. Heat may also
be maintained by immersion-type elec-
tric heaters, by releasing steam into the
water, or by gas burners under the bot-
tom of the metal tank. With a little prac-
tice, the temperature can be kept within
a half degree above and below the de-
sired temperature after initial adjust-
ment; such regulation is necessary for
the best results. Water circulation in a
large tank is best achieved by a circulat-
ing pump or by a submerged propeller.
Circulation is essential during heat
treatment to prevent temperature strati-
fication and to promote heat penetration
into the material.
Thermometers must be accurate at the
range 120° to 135° F (see Appendix) ;
it is usually desirable to have two or
three of them suspended in the tank to
indicate degree of temperature uni-
formity in the water. It is a worth-while
precaution to have a precision-calibrated
[ 224 ]
Fig. 110. Commercial hot-water treatment tank for bulbs, ornamentals, and strawberries. Tem-
perature is thermostatically controlled, and the water is agitated by a propeller.
thermometer (accurate in the above
range; see Appendix) , against which the
others may be calibrated at the exact
temperature used. Thermometers with
expanded scales in the critical treatment
ranges are available in brass protective
cases (see Appendix). These provide
precise temperature measurement several
degrees either side of a specified point.
Since they are reasonable in price, they
should be more commonly used.
For small quantities of seed or plants
we have had uniformly good results us-
ing a 20-gallon sink or tub, maintaining
uniform temperatures by a trickle of hot
water, and stirring with a wooden
paddle.
The material to be treated may be
placed in open-weave plastic or cloth
bags, or in screen boxes for ready han-
dling. Seed in cloth bags should be
gently kneaded by hand to expel air
bubbles; material in screen boxes should
be constantly agitated for the same pur-
pose.
The treatment should be accurately
timed so that exposure to heat will be
precise.
Cooling
Prompt cooling of the treated material
is imperative in order to increase pre-
cision of timing exposure. This may be
achieved by turning a hose on the con-
[225]
tainer, or by dipping in a tank of cool
tap water, again kneading for rapid heat
transfer. This should be continued until
the material reaches water temperature.
The tank, and the water in it, must be
free of pathogens; it should not have
been used for soaking untreated material.
Drying
The seed or stock (except foliage
plants) should be dried as rapidly as
possible, certainly within a few hours.
This is best accomplished by spreading
on screens, treated cloth, or new papers
over which a warm dry current of air is
blown, and which are raised off the
ground. Temperatures in this phase
should not exceed 90° F, so that drying
is accomplished by a large volume of dry
air rather than by heat. The screen may
be disinfested with a formaldehyde solu-
tion (1 gal. commercial strength to 18
gal. water), followed by a water rinse,
or by a sodium hypochlorite spray (0.4
per cent available chlorine) as explained
in Section 12.
Storage
Handling and storage of the clean ma-
terial must conform to rules of sanita-
tion. Under no conditions should the
material be placed in old contaminated
boxes, trays, or bags, or handled with
dirty tools; these implements should be
sterilized before re-use (sees. 3 and 12).
Growing in isolation
The clean material must be grown
isolated from the general propagation,
to minimize opportunity for contamina-
tion.
Application to specific
nursery crops
The above methods are perhaps best
presented in relation to specific crops
and diseases. Only the treatment phases
mentioned are needed in each case.
Aglaonema* — against Rhizoctonia
and water molds. Old cane will stand
Previously unpublished data of the authors.
treatment at 120° F for 30 minutes;
cool; plant.
Aloe — against water mold (Pythium
ultimum) root rot. Plants of various
sizes cleaned of debris, treated at 115°
F for 20 to 40 minutes (the larger the
plant the longer the time) ; cooled;
planted. Almost completely effective in
salvaging infected plants; injury mini-
mal (fig. 111).
Apium (celery) — against late blight
(Septoria spp.) in seed. Treat seed at
120° F for 30 minutes; cool; dry; plant.
Treatment of seed does not appreciably
reduce stand. Healthy plants produced
from treated seed require less spraying
in the field, as the pathogen builds up
slowly from field debris.
Begonia, tuberous — against root-knot
nematode. Tests by P. A. Miller3 indi-
cated that treatment of dormant tubers
at 120° F for 30 minutes freed them of
nematodes without injury. Cool and
plant.
Buxus (boxwood) — against root-knot
nematode. Tests by P. A. Miller3 indi-
cated that treatment of bare-root plants
at 118.4° F for 30 minutes freed them
from the nematodes without serious in-
jury. Cool and plant.
Caladium — against Sclerotium rolfsii
tuber rot. Florida studies found that
treatment of dormant tubers at 122° F
for 30 minutes eliminated the organism
without injury. Cool and plant. In Cali-
fornia, a bacterial soft rot of the rhi-
zomes is not controlled by this treatment.
Capsicum (pepper) — against Rhizoc-
tonia in seed. Treat seed at 125° F for
30 minutes; cool; dry; plant. Com-
pletely effective with almost no reduction
of germination.
Dieffenbachia* — against water molds,
bacterial leaf spot, and bacterial soft rot.
Important that hardened canes be used
as they tolerate the necessary 125° F;
others stand only 120° F; young leafy
shoots will not survive treatment. Treat
:| Department of Plant Pathology, University
of California, Los Angeles.
[226]
Z^Sl-SjiWi'eySy ■';.''Zi''!'Xi!'f^^f.
Fig. 111. Control of Pythium root rot of Aloe variegata by hot-water treatment at 115°F for
20 min. A, Treated plants above and checks below, 20 days after planting. B, Treated plant at
left and check at right, 100 days after planting, showing the rapid recovery after treatment
and planting in treated soil.
cane in pieces about 2 feet long at 125°
F for 30 minutes; cool; hold canes in
steamed sphagnum moss until roots or
buds start; cut into pieces each with a
single bud, plant immediately in perlite
and peat; replant in soil when top is well
started. Has given excellent control. In-
creases percentage of buds of D. bausei
and D. picta breaking dormancy, as for
Syngonium podophyllum below. Tip
cuttings from treated plants, grown with-
out overhead sprinkling, should further
insure freedom from pathogens. There is
some evidence that soft-rot bacteria may
be spread through the propagating bed
by larvae and adults of fungus flies.
Spraying the soil surface with dieldrin
(wettable powder, 1 oz. per 7% gal.
water) or malathion (wettable powder,
2 oz. per 7^2 gal. water) has given some
promise in controlling these insects.
Fittonia* — against Rhizoctonia (fig.
112) and water molds. Harden plant.
* Previously unpublished data of the authors.
Clean and treat whole plant at 124° F
(120° if plant is unhardened) for 30
minutes; cool; make cuttings and divi-
sions, removing any damaged leaves;
plant at once in perlite and peat, where
roots may form in less than a week.
Leaves are very sensitive to treatment,
but stems survive and new shoots de-
velop. See Section 16 for the experience
of one grower with this treatment.
Gerbera — against root-knot nematode
(Meloidogyne incognita) . Tests by S.
A. Slier4 indicated that treatment of
bare-rooted plants at 118° F for 20 min-
utes freed them from these nematodes.
Treated plants started a little slowly, but
surpassed the untreated ones after 5
months.
Haworthia — methods and results simi-
lar to those with Aloe.
Lilium (Croft) — against Rhizoctonia,
stem and bulb nematode, and root-lesion
4 Department of Plant Nematology, Univer-
sity of California, Riverside.
[227]
Fig. 112. Stem cuttings of Fittonia verschaffeltii var. argyroneura in a treated rooting medium
in a propagation case, showing effectiveness of control of Rhizoctonia by hot-water treatment.
Above, cuttings treated at 120°F for 30 minutes; note the perfect stand and absence of leaf
decay. Below, untreated cuttings from the same lot, showing leaf decay and poor stand.
[228]
nematode; ineffective against Fusarium
basal rot. Tests by J. G. Bald and P. A.
Chandler5 showed that the following
schedule was successful for obtaining
useful commercial stock: Cure bulbs at
95° F and 95 per cent humidity for 1 to
2 weeks; presoak 2 days in cool water.
Treat for 2 hours in water plus formalde-
hyde (1 gal. 37 per cent commercial for-
maldehyde per 200 gal. water) at 115°;
cool. Aftersoak the bulbs in Puratized
Agricultural Spray (1 pint per 125 gal.
water) for 24 hours. Scale the bulbs and
dust scales with ferbam; place on moist
vermiculite at 75° and 95 per cent hu-
midity. Remove bulbils and plant in
treated soil.
Matthiola (stock) — Seedsmen now
treat seed they plant so as to produce
seed free from bacterial blight. Seed is
treated by the producer in plastic screen
bags at 130° to 131° F for 10 minutes;
cooled; and dried. Special techniques
are necessary in handling because of the
mucilaginous seed coat. Most stock seed
is now free of bacterial blight owing to
the success of the treatment.
Pellionia* — methods and results simi-
lar to those with Fittonia. Plants tolerate
treatment well, develop strongly.
Philodendron pertusum and P. corda-
tum* — against bacterial stem rot of the
former, and Rhizoctonia on the latter
(fig. 114). No data available on effect of
hardening, but both plants take 120° F
for 30 minutes well. Discarded, hard-
ened, conservatory plants seem to take
the treatment very well. Treat; cool;
root in steamed sphagnum (as with Dief-
fenbachia) ; cut into propagating sec-
tions of 1 to 2 buds.
Rosa — against dagger (Xiphinema)
and spiral (Helichotylenchus) nema-
todes in Florida; wash roots; treat at
121° F for 3% minutes; cool; dry. If
root-knot or root-lesion (Pratylenchus)
5 Department of Plant Pathology, University
of California, Los Angeles.
* Previously unpublished data of the authors.
nematodes are present, 121° to 123° for
10 minutes is required.
Strelitzia — against root-rot complex
involving internally borne Fusarium
moniliforme. Presoak seed 1 day in water
at room temperature; treat at 135° F for
30 minutes; cool; dry; plant. Commer-
cially effective in preventing loss of seed-
lings without reducing germination.
Syngonium auritum (Philodendron
trifoliatum) — against black cane rot
(caused by a specialized form of the
fungus Ceratocystis fimbriata) . Harden-
ing increases heat tolerance of plants.
Treat whole bare-rooted plants at 120°
F for 30 minutes; cool; plant in soil.
Eliminates pathogen; some leaf injury,
but plants quickly recover.
Syngonium podophyllum* — canes are
treated in pieces about 2 feet long ; toler-
ate treatment without injury. Clean and
treat at 120° F for 30 minutes; cool;
handle as for Fittonia. This treatment
breaks dormancy of the cane buds,
greatly increasing the rapidity and suc-
cess of propagation (fig. 113). Present
procedure is to hot-water-treat as above,
then hold in a humidity cabinet at 70° F
for 2 to 3 weeks before planting.
Weigelia — against root-knot nema-
tode. Tests by P. A. Miller6 indicate
that treatment of bare-root plants at
120° F for 30 minutes freed them of
nematodes without serious injury. Cool
and plant.
Zantedeschia aethiopica (white calla)
— against water mold {Phytophthora
richardiae) . Clean dormant rhizomes;
treat at 122° F for 1 hour; cool; dry.
Zinnia — against Alter naria disease
(A. zinniae) and Rhizoctonia. Seed
should not be more than 1 year old, or
germination will be reduced by treat-
ment. Treat seed at 125° F for 30 min-
utes; cool; dry. Commercially effective
in eliminating these pathogens from
fresh seed, without serious injury.
6 Department of Plant Pathology, University
of California, Los Angeles.
[229]
Fig. 113. Effect on growth of Syngonium podophyllum (Emerald Gem) stem cuttings of hot-
water treatment (120°F for 30 min.) and holding under humid conditions and 70° for 2 weeks.
Photos, after 7 weeks' growth in the glasshouse, show stimulation of bud and root development
due to breaking of dormancy. Upper left, untreated check, planted at once in the glasshouse.
Upper right, untreated check, held at 70°. Lower left, treated and planted at once in the glass-
house. Lower right, treated and held at 70°.
Chemical Treatment of
Planting Stock
This method is effective only against
pathogens externally carried on the
planting material where the chemical
will come in contact with them. It is,
therefore, of limited value to nursery-
men.
Nurserymen should realize that chemi-
cal seed treatments are of two types
(protective and eradicative), only one of
which aims at elimination of disease
organisms from the seed. It is a potenti-
ally disastrous misconception that the
"treated" seed sold in packets today is
free of pathogens. The seed is treated
with a protective mild fungicide (for ex-
ample Spergon on sweet pea seed) to
protect it from decay prior to emergence,
or to reduce damping-off in slightly in-
fested soil. Treatments that eradicate
pathogens from seed usually reduce
germination, and therefore are not ap-
plied before sale. Three examples of
eradicative chemical treatment may be
cited.
1. Dormant white calla rhizomes are
soaked for 1 hour in formaldehyde (1
pint to 6% gal. water), mercuric chlo-
ride (one 7^/2 grain tablet per pint of
water), or in a suspension of 8 ounces
New Improved Ceresan plus 1 ounce
Dreft per 25 gallons of water. This will
free them of the root rot Phytophthora.
Since growth may be somewhat delayed
by these treatments, the heat method de-
described above may be preferable.
2. Seed of China aster may be treated
| 230 ]
Fig. 114. Control of Rhizoctonia root rot of Philodendron cordatum plants grown on poles in
pots. Plants shown above are in the soil ball; the same plants are shown below with roots washed
free of soil. Plants at left as they were obtained from a commercial nursery, showing severe root
decay; comparable plants at right 3 months after the root systems and the poles were washed
free of soil, treated in hot water (120°F for 30 min.) and replanted in treated soil.
[231]
with an unheated mercuric chloride solu-
tion (one l1/-! grain tablet per pint of
water) to free it of the wilt Fusarium. A
given volume of seed is placed in a jar,
covered for 30 minutes with three times
that volume of mercuric chloride and
intermittently shaken. The solution is
poured off, the seed rinsed with several
changes of water, and dried. Some germi-
nation reduction may result, particularly
in seed with cracked coats.
3. The foliar nematode (Aphelen-
choides ritzema-bosi) of chrysanthemum
may be eliminated from a cutting bed
by chemical treatment. A spray of para-
thion (25 per cent wettable powder, 1
lb. per 100 gal. water, plus 4 to 6 fl. oz.
Triton B-1956) will be absorbed by the
plant and poison the nemas. Formerly
sodium selenate applications to the soil
were used for the same purpose. Sodium
selenate or Demeton (Systox) are used
to free Saintpaulia of foliar nematode.
Sanitary Measures
It is rarely possible to free stock of a
pathogen by removal of diseased tissue.
However, azalea plants may be freed of
the flower-blight fungus, Ovulinia aza-
leae, by carefully removing all dead
flowers from the plant, and stripping off
the top inch of rooting medium, or by
bare-rooting the plant. Thus, carryover
sclerotia are eliminated, breaking the
pathogen's cycle.
Similarly, the flower-blight fungus
(Sclerotinia camelliae) of camellia may
be eliminated by careful removal and
burial or burning of flowers. If no
flowers are permitted on young nursery
stock, and not allowed to fall into the
cans from large flowering plants, there
can be no carryover of the fungus with
the plants. Removal of the top inch of
soil, as for azalea, will be similarly ef-
fective.
Aging of Seed
Rarely the fungus will survive for a
shorter period of time than will the
plant seed in which it developed. It is
possible to free celery seed of the late-
blight Septoria by holding it for 3 years
or more before planting. This procedure
is applicable only on celery seed among
the nursery crops.
Prolonged Roguing of Diseased
Plants from a Stock
Diseases have periods when they may
not be detectable in plants that later may
show striking symptoms. This makes it
impossible to eliminate infected plants
by a single roguing. If, however, the
causal agent has essentially no natural
spread, it is possible by careful and re-
peated roguing over a period of several
years to clean up a stock and thus estab-
lish a healthy mother block. This is true
of many of the viruses of woody plants,
as for example, rose mosaic.
If the virus spread occurs only with
budwood or scions it is possible to index
plants and issue registered budwood
from disease-free specimens. This is
being done for citrus stock free of psoro-
sis virus, and for some of the stone
fruits.
Virus-indexing Methods
Recognition of virus infection is diffi-
cult in plants which, for various reasons,
temporarily or permanently fail to show
symptoms. To find virus-free plants
under these conditions, special indexing
procedures are required. Such methods
are highly technical, but are already in
commercial use by specialist propa-
gators. Brierley and Olson (1956) have
described a method for graft-indexing
chrysanthemums to highly susceptible
healthy varieties in order to detect virus-
infected plants. Only the virus-free plants
are then propagated. Gasiorkiewicz and
Olson (1956) have described a similar
method for carnations. The presence of
mechanically transmissible viruses of
either plant may be detected by sap
transfer, usually by the use of carbo-
rundum powder, to the leaves of some
host which shows symptoms. With some
[232]
viruses (aster yellows) the use of an ap-
propriate insect vector is necessary.
Growing Plants from Seed
Disease agents frequently are not car-
ried through the seed but rapidly build
up through vegetative propagation. This
is particularly true of viruses. Thus,
raising ranunculus, anemone, and free-
sias from claws, roots, or corms leads to
serious losses from mosaic, whereas the
loss is minimal when grown from seed.
Similarly, yellow calla grown from true
seed is free of bacterial soft rot, water
molds, and Rhizoctonia, all of which are
commonly carried on the rhizomes. Ap-
parently it is possible to obtain ferns
free of foliar nematode (Aphelenchoides
fragariae) by starting with spores from
leaves kept dry during growth.
Selecting the Growing Region
The semiarid California climate is an
effective ally in eliminating many nurs-
ery diseases because plants dry off
quickly after rain or overhead watering.
Many fungi require prolonged moist
conditions in order to produce spores,
which may in turn be spread only in
water and must be wetted for a few to
48 hours to infect the host.
Many diseases, important elsewhere,
are essentially unknown here because of
the climate, among them snapdragon
anthracnose and Phyllosticta leaf spot,
Phomopsis canker of aster, bacterial leaf
spot of poppy, and Ascochyta flower
blight of chrysanthemum. Septoria leaf
spot of chrysanthemum is important
only in propagating frames or plantings
extensively watered from above. Seed of
China aster free of Stemphylium calli-
stephi, and zinnia free of Alter naria zin-
niae may be produced in California by
growing in dry inland, instead of coastal,
valleys. Azalea and camellia flower
blights largely occur in California
under lath or shrubbery cover. Promot-
ing air movement through the lath house
by removal of the sides will reduce the
disease by restoring conditions of rapid
drying.
Although there are few nursery dis-
eases that can be eliminated solely
through selection of the region, growers
should exploit this climatic advantage of
the state to the maximum in support of
other controls.
Seed or plants grown under dry condi-
tions without overhead watering often
are freest from disease. They should be
grown-on without sprinkling or syring-
ing whenever possible.
Reporting Diseased Stock to
the Propagator
This point is important because it is
sometimes the primary force in bringing
about improvement. Propagators may
actually be unaware of the situation and
may be grateful for notification of it, or
they may mistakenly think that since
perfection is unattainable, a fairly clean
stock is good enough. They can no more
have "a little disease" than they can be
a little dead! They will, in any case, cer-
tainly respond faster to customer pro-
tests than to advice from Agricultural
Experiment Station workers or state
nursery inspectors. In this democratic
process of the business world, the grower
who accepts diseased stock without pro-
test is derelict of his duty in the system.
Since in the long run results may be
achieved in this way that apparently can-
not otherwise be accomplished, there is
little virtue in being a silent sufferer.
Of the rare propagator who inten-
tionally markets diseased stock little
need be said, since he is self-exterminat-
ing. If he clips the scattered galls of root-
knot nematode from his rose roots or
cuts out the swellings of bacterial fascia-
tion from his divisions of Esther Read
daisies before shipment, he is practicing
fraud rather than disease control, and
this will eventually be recognized by his
customers.
[233]
MAINTAINING CLEAN STOCK
Once healthy nursery stock is ob-
tained, one faces the problem of main-
taining it in this condition. In actual
practice, clean stock is fairly commonly
obtained but is so quickly infected that
the grower does not become aware of its
value. New seedling varieties are almost
always free of virus diseases as well as
most pathogens, and in this sense plant
breeding is a primary source of healthy
stock. Usually no effort has been ex-
pended to maintain the variety in this
condition, and it is soon discarded be-
cause of disease; the rapid commercial
disappearance of the King Cardinal
carnation because of mosaic is but one
of many instances of this sort. This loss
more often results from lack of knowl-
edge concerning the desirability of, and
methods for, maintaining the healthy
condition of the plants than from in-
surmountable difficulties in the system.
For example, a large eastern propagator
is developing and introducing new seed-
ling varieties of carnations that are free
from most of the major diseases. They
are maintaining stock of these varieties
under conditions that largely prevent
their becoming diseased. Growers buy-
ing such a variety sometimes find that
it develops "excessive growth" the first
year (in large part because of freedom
from disease) , and usually note that pro-
duction drops in a few years under their
own propagation. They then buy new
cuttings of the variety and start over.
This company keeps the variety disease-
free, rather than permitting it to become
infected (as the grower and the propa-
gator have done in the past), so that
there is now a clean stock to fall back on.
The more important basic procedures
for preventing contamination of stock
are given below.
Isolating New Stock
Almost every nurseryman has known
an instance in which a small quantity of
new stock was purchased and set among
healthy local plants, introducing disease
to the whole lot. A few progressive
growers have an "isolation ward" or
greenhouse to which new stock is sent
until freedom from disease is established.
Such a practice has the full weight of
scientific theory and bitter experience
behind it. The marvel is that it is not
more frequently used.
This process is used in addition to any
inspection and certification practices.
Many diseases are not detectable at first
by inspection because there is always a
lag (called the incubation period) be-
tween infection and symptom appear-
ance. Snapdragon rust, for example,
shows no symptoms for about a week
and is not conspicuous for 10 to 14
days. Other diseases may appear only at
certain stages of growth, as for example,
azalea and camellia flower blights dur-
ing blooming. Still other diseases (for
example, geranium mosaic) may be
evident for only brief periods and then
disappear. The safe procedure is, there-
fore, to isolate introduced plants until
their health is established. Because of the
complexities exemplified above, the
grower should consult the local farm ad-
visor or the Agricultural Experiment
Station in arranging a program of this
sort. Another reason for using pathogen-
free stock is that it may be brought into
a nursery without preliminary isolation.
The use of a "pest house" is highly
desirable in most nurseries, and is abso-
lutely required in one that is raising
pathogen-free stock for sale. Because
some pathogens or viruses are carried
by wind and insects, it is essential that
the isolation house really be separated
from the main plantings.
The same principle may be involved
in the handling of single plants. Thus,
callas are commonly grown in pots
I 234 ]
rather than benches in order to prevent
the spread of Phytophthora root rot and
bacterial soft rot.
Isolating Propagative Operations
At first seedlings are quite free of
virus infection, gradually accumulating
viruses with time. It is important to de-
lay such infection by not locating a seed
or cutting bed near any source of infec-
tive insects.
Thus, raising delphinium seedlings
near an old planting of delphinium or a
growing celerv field is an invitation to
leafhoppers. They carry the aster-yellows
virus and. in feeding, infect the seed-
lings; symptoms may not appear, how-
ever, until the plants are growing in
home yards. Such seedbeds might well be
tightly covered with aster cloth or plastic
screens.
Seedlings of aster, tomato, and pepper
raav be infected with the spotted-wilt
virus through migration of thrips from
surrounding infected plants. In one in-
stance tomato seedlings were thus in-
fected from old diseased dahlia plants
grown bv the nurservman's wife for
cut flowers just outside the glasshouse
ventilators. Certain coastal areas have
severe outbreaks of spotted wilt each
vear. These "endemic areas" are located
in the cool coastal fog belt, and have a
persistent population of dahlias, nas-
turtiums, callas, buttonweed, chickweed,
and other hosts. Such endemic areas
should be avoided for propagation of
certain plants.
Growing stock seedlings in an area
surrounded by wild radish and mustard
is another dangerous situation. Aphids
carry mosaic to the stocks, which may
not show symptoms until flowering.
In general, propagative activities
should never be conducted in a weedy-
area or in one with near-by fields of
virus-infected herbaceous crops. Because
of the complexities involved, consult
your farm advisor for details in specific
cases.
The Mother-Block Principle
When one has purchased or developed
healthy stock, it should be grown in
isolation and with special care. To main-
tain this material in a separate planting
is the mother-block principle. It is ob-
viously easier to prevent introduction of
a pathogen into a small special block of
stock than into large plantings. It is
easier to isolate such a small nucleus
planting, to inspect it carefully and re-
move any diseased plants, and to control
insects that may spread virus diseases.
The job is, therefore, more likely to get
done.
There should be only one-way traffic
with the established mother block; cut-
tings or plants may be taken out but no
plants should be brought into it (fig.
115). Above all. no buds or grafts
should be placed in plants of the block;
undetected viruses and V erticillium wilt
can thus be introduced and ruin the
planting. Visitors should not be per-
mitted in the glasshouses containing the
mother blocks.
By carefully selecting within mother-
block plants, one can prevent both loss
of horticultural quality and increased
variation, and may thus be able to effect
distinct improvements. The maintenance
of the mother block, and the selection of
plants in it, should be under the personal
supervision of the owner, never referred
to routine help. Growers who do not
maintain mother blocks often sell the
best stock in an effort to please their
customers, and then plant the remainder
for next year's propagation. Because
many diseases cause decreased plant size
and vigor, such a practice may actually
be selecting toward disease. The phe-
nomenon of "running out" of horticul-
tural varieties probably largely repre-
sents such accumulation of disease and
weak variants. The production and mer-
chandising of plants, and the mainte-
nance of the basic stock for future propa-
gation, must be handled as independent
[ 235 ]
' '*,
a
Pathogen-free stock obtained from:
Chance healthy plants
New seedlings
Practices which enable plant
to grow away from pathogen
Cultured-cutting technique
Heat treatment
Chemical treatment
Sanitary practices
Selected growing areas or conditions
>F
Propagate
and grow
Careful check
for freedom
from pathogens
Establish isolated
permanent mother
blocks
Healthy
— ^ propagating
stock sold
a
o
3
TJ
O
E
E
o
u
Propagate,
plant,
and grow
Crop "* Propagate,
pro- ^ — plant,
duction and grow
Grow on
V_ for crop ^_ __ _
Check for
freedom from
pathogens
before each
propagation
Propagate
from plants z.
if healthy
+
Grow a single crop, and
discard plants.
Grow in isolation for single
early propagation.
Plant to establish temporary
mother block. Must be
isolated from commercial
production.
Grow for crop
Fig. 115. Diagram showing the segregation of propagation and commercial production, and
the sequences of operations that may be followed. Only in the last method (not recommended;
used only in exceptional cases) is propagating material taken from commercial production stock.
Commercial growing activities shown in boldface type, stock propagation in ordinary type.
Treated soil and containers to be used throughout. See text for details and specific crops.
and isolated activities. To do so is a
long-term service to the nursery indus-
try, the grower, and his customers.
An example of the danger of not hav-
ing a mother block of rootstock may be
cited. A nursery budded one of its new
hybrid rose seedlings on three under-
stocks taken from a commercial field
and, after the plants were established,
the seedling was lost. Buds taken from
these three plants were placed in a field
increase-block. A large percentage of the
plants developed variegated symptoms
of yellow mosaic, and it was found that
two of the three original plants had been
infected from the rootstocks. It was
CAUTION: Many of the chemicals
mentioned in this manual are poi-
sonous and may be harmful. The
user should carefully follow the pre-
cautions on the labels of the con-
tainers.
necessary to destroy all detectably in-
fected plants and delay introduction for
another year. The world thus narrowly
missed losing what proved to be a fine
Ail-American rose.
Sanitary Procedures
This principle for maintaining healthy
stock is less specific than the foregoing,
and therefore more difficult to apply. It
is, however, of the utmost importance
that careful sanitation be practiced. A
number of procedures have been out-
lined for this, and are summarized in
"A Nursery Sanitation Code," Section 1.
The essence of a successful sanitation
program is the positive mental attitude
of the grower. One should analyze the
many nursery operations for potential
"leaks" of contamination and eliminate
them before trouble appears, rather than
wait until the appearance of disease
forces corrective measures. This manual
provides information necessary for such
analysis.
[ 236 ]
SECTION
0 m
i
Beneficial Soil
Microorganisms
John Ferguson
Microorganisms in the soil
Transformation of plant nutrients by microorganisms
Effect of soil treatments on microorganisms
Controlled colonization: a future step
Xhis section deals with the numerous
biological, physical, and chemical proc-
esses in the soil which result from the
activities of microorganisms. An at-
tempt is made to portray briefly the soil
microbiological population, the interre-
lations among microorganisms, the
microbial transformation of various ele-
ments essential for plant growth, the ef-
fect on plant disease and nutrition of
man's activities in modifying the soil
population, and the general applications
of this knowledge to the growing of
better plants.
One of the essential functions of soil
organisms is decomposing organic mat-
ter and converting to forms available to
crop plants such elements as carbon,
nitrogen, calcium, magnesium, potas-
sium, phosphorus, sulfur, iron, and zinc.
There are only limited sources of several
of these elements, especially carbon,
nitrogen, and phosphorus, in a form
available to plants. These essential ele-
ments must be returned to inorganic,
available forms, a process carried out
primarily by the soil population. Thus,
through their various activities, soil
microorganisms enable life to continue
by keeping in constant circulation the
elements most essential for plant and
animal life.
MICROORGANISMS IN THE SOIL
Abundance terial in normal field soil there are about
Untreated natural top soil has a vast 10 pounds of microorganisms. Soil fungi
population of microscopic plants and alone consistently occur in quantities
animals. The members of this extremely weighing 1,700 pounds per acre, and
active population include many forms of they are only one of the numerous repre-
life. For every 100 pounds of plant ma- sentatives of the soil community. Bac-
[237]
teria commonly occur in amounts of 30 tain plant parasites may persist in soil
to 40 pounds per acre, each pound com- for several months, however, and some
prising upwards of 500,000,000,000 in-
dividual bacteria. (Five hundred to 1,000
bacteria placed in a line would extend
across the head of a pin.) It is interesting
that another group of microbes very
similar to bacteria, the actinomycetes,
occur in high enough concentrations to
give soils their typical musty odor. Most
of this vast microbial population is con-
centrated in the upper 1 to 3 feet of soil,
the depth depending upon the environ-
ment and nutrient availability.
Competition
Soil may well be likened to a minia-
ture jungle in which some species prey
upon others and all compete for avail-
able space and nutrients. All forms of
microscopic life (including bacteria,
fungi, actinomycetes, algae, nematodes,
and protozoa) exist in the soil in a state
of dynamic equilibrium, or ever-chang-
ing balance. Any change, such as in food
supply or environment, affects all mem-
bers of the colony and, therefore, dif-
ferent species become dominant from
time to time. Any new addition to this
population faces intense competition and
often perishes or develops slowly until
some factor shifts to its advantage. Thus
for any so-called "microbial inoculant"
to be effective, the environment must be
favorable and a ready nutrient source
must be available.
Relation to Crop Plants
Parasites and saprophytes
In their relation to plants, micro-
organisms can be considered as either
parasites or saprophytes. The parasitic
forms are capable of growing on the liv-
ing plant and causing its decreased
growth or death. Saprophytic microor-
ganisms grow only on dead tissue or its
decomposition products. The typical soil
population consists of organisms which
arc largely saprophytic in nature. Cer-
[238]
are capable of leading a normal exist-
ence there. In water molds, for example,
the parasitic activity may be relatively
unimportant for the survival of the or-
ganism, and only incidental to its normal
saprophytic life.
Within one species of the fungus
genus Fusarium are purely saprophytic
forms and highly specialized vascular
parasites capable of saprophytic sur-
vival. This illustrates the escape from
competition achieved through the spe-
cialization of parasitism. As a sapro-
phyte an organism must compete with
the majority of the soil population for
the available organic matter and mineral
elements, while as a parasite capable of
penetrating a living plant, most of the
competition is eliminated. The parasite
damages the plant not only through its
own activities, but also by providing an
entrance for secondary organisms ca-
pable of damaging the plant but unable
to penetrate alone.
Direct and indirect effects
The number, kinds, distribution, and
interrelations of soil organisms have a
very decided effect on plant growth.
Within this delicately balanced complex
are organisms favorable to plant growth
and those which affect growth adversely.
Included in the group which directly
favor plant growth ("beneficial," fig.
116) are, for example, microbes which
aid in making essential nutrients avail-
able, decompose toxic materials, or im-
prove soil structure. Organisms which
inhibit plant growth ("harmful," fig.
116) may do so either by direct attack,
as with parasites or predators, by com-
petition for space or nutrients, or by the
release of toxic substances.
As illustrated in figure 116, the harm-
ful or the beneficial organisms are in
turn affected, either favorably or ad-
versely, directly by other microbes or
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Beneficial to the plant-
beneficial organisms — thus
beneficial to the plant.
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BENEFICIAL ORGANISMS
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indirectly through a series of organism
reactions. All soil microbes thus ulti-
mately contribute to either the increase
or decrease of plant growth.
Directly beneficial organisms are
those which attack organic matter and
rehase elements in a form available for
plants, for example, ammonifying and
nitrifying bacteria.
Directly harmful microbes are repre-
sented by plant pathogens such as
Rhizoctonia solani or V erticillium albo-
atrum.
The soil fungus Trichoderma, which
attacks Rhizoctonia, is a good example
of an indirectly beneficial organism. The
nematode-trapping fungi also illustrate
the indirectly beneficial effect.
An organism antagonistic to Tricho-
derma would represent a harmful agent
working several steps removed from the
plant since a reduction of Trichoderma
could cause Rhizoctonia damage to in-
crease and thus decrease plant growth.
There are numerous cases where organ-
isms attack other organisms, change pH,
or tie up essential elements, and the re-
sulting shift in the soil community
markedly affects the plant. These will be
illustrated further in the section, and
work will be described in which bene-
ficial organisms were used to reduce
disease loss and to make nitrogen more
readily available.
Distribution of Microorganisms
The distribution of the types and
numbers of organisms comprising the
complex soil population is controlled by
the nature and availability of nutrients,
the physical and chemical properties of
the soil, and the environmental condi-
tions, especially aeration, temperature,
and moisture supply. Because of their
extremely small size, tremendous abun-
dance and power of multiplication, and
wide variability in growth requirements,
microbes are universally distributed in
nature.
Concentration in surface layer
Microorganisms occur in largest num-
bers in the surface layer of soil, which
varies in thickness from a few inches to
several feet. The greatest abundance and
variety of individuals are found either
at the very surface of soils (for example,
soils covered with litter in forests,
meadows, or other shaded areas) or just
below the surface as in regularly culti-
vated fields.
Effect of organic matter
The numbers of microorganisms de-
crease with depth, the amount of decrease
varying with soil conditions, especially
the distribution of organic matter and
the degree of aeration. The numbers,
types, and activities of microorganisms
fall off rapidly in shallow soils deficient
in organic matter. An excellent example
is the wind-blown soils recommended for
the U. C. soil mixes. As few as 17,000
organisms per gram have been reported
from such soils containing about 0.3
per cent organic matter. These organ-
isms were largely bacteria. The same
type of soil with 0.45 per cent organic
matter gave an average of 60,000 organ-
isms per gram. Common agricultural
soils containing 3 to 5 per cent organic
matter have from 1,000,000 to 500,000,-
000 organisms per gram. These facts
show the close relation between organic
matter and soil microorganisms.
Concentration in the
rhizosphere
The rhizosphere is the name given to
that area of soil immediately around
and on plant roots, which supports in-
creased microbiological activity. There
are from three to fifty, times as many
organisms in the rhizosphere as in soil •
not closely associated with plant roots.
This increased activity in the root area
varies with different plants and is char-
acteristic of any given species. For ex-
ample, corn is typically high in numbers
[240]
of organisms in the root area, while
some of the grasses are comparatively
low. Organisms in the rhizosphere are
greatly influenced by plant roots in re-
spect to both kinds and number, and
constitute a definite and unique micro-
population.
Nutrient Requirements
Dependence on green plants
The nutritional requirements of mi-
croorganisms are much the same as
those for higher plants. Most soil micro-
organisms except algae, however, lack
the ability exhibited by green plants to
manufacture organic substances from
inorganic elements in sunlight. There-
fore, the majority of soil microbes are
dependent for their nutritional and
energy sources upon the decomposition
of the complex soil organic substances
which come directly or indirectly from
green plants. In attacking organic matter
as a food source, soil microorganisms
bring about various changes which
liberate plant food in forms available to
higher plants.
Since the activities of soil microor-
ganisms are so closely associated with
but completely unavailable to others.
The soil population shifts, a succession
of different forms predominating as the
food materials are decomposed and
their chemical constitution changed.
Thus, organic-matter breakdown sup-
ports a sequence of organisms, each ef-
ficient in utilizing specific degradation
products. Because of this great diversity
of organisms a soil population can digest
nearly any material supplied to it. When
microorganisms decompose a substrate,
many of the essential elements are used
to form the material of their developing
cells. These materials are thus rendered
unavailable to the plant until the organ-
isms die and are decomposed by other
microorganisms.
Rate of decomposition
As an example of the rapidity of trans-
formations by organisms, in a few hours
sugar can be completely decomposed to
carbon dioxide and water, or protein to
ammonium, carbon dioxide, water, and
other compounds. The extent to which
microorganisms develop is limited by
the nutrient substrate, environmental
conditions, and the formation of certain
products injurious to their activities.
the growth of higher plants, efficient soil Although modifications in the supply of
treatment to kill pathogens requires an
understanding of these activities so as
to capitalize on them. Many conditions
resulting in unfavorable plant growth
could be avoided or quickly overcome
if, in the treatment of soils, the activities
of soil microorganisms were considered
to the extent that the effects on higher
plants are.
Steps in decomposition
of organic matter
The complete breakdown of organic
matter by microbes requires numerous
steps and many types of organisms. Soil
organisms differ greatly in their ability
to attack a given substrate. When an
organic material is added to the soil it is
immediately available for some species,
oxygen, moisture, and inorganic com-
pounds, or a change in temperature may
affect the development of the soil popula-
tion, the greatest response in activity is
accomplished by the addition of organic
substances to the soil or bv treatments
which destroy part of the soil popula-
tion. An example may be cited from
Waksman and Starkey (1931), who
stated that when a ton (dry weight) of
fresh organic matter, such as manures or
plant stubble, is worked into soil the
microorganisms immediately become
active. First, the water-soluble substances
are decomposed, then the starches, the
proteins, and cellulose. Within 10 to 20
days, under favorable conditions, onlv
about 1,000 to 1,200 pounds may be left
out of the 2,000 pounds originally added.
[241]
Our experience with hoof and horn meal,
peat, or wood shavings indicates a much
slower breakdown with these materials.
This is one of the reasons why leaf mold
and manure are not used in the U. C-
type mix.
Carbon nitrogen ratio
Much can be interpreted regarding
end products which will be formed and
the speed of their formation if the organ-
isms effecting the decomposition of an
organic material, the composition of the
material, and the environment are
known. Fungi use the organic nutrients
as a source of energy and of carbon.
They use for synthesis of their cells an
average of 40 per cent (a range of from
10 to 65 per cent reported by most
workers) of the carbon contained in the
organic compound decomposed. The re-
mainder of the carbon goes off as carbon
dioxide or is left as incompletely de-
composed material. Bacteria and actino-
mycetes (in the presence of normal
amounts of oxygen) assimilate an aver-
age of 25 per cent of the carbon con-
tained in the decomposed organic mate-
rial (table 18).
Accompanying the carbon assimila-
tion, appreciable amounts of nitrogen
are used in the formation of cell pro-
teins. The carbon content of microbial
cells averages about 50 per cent of the
dry weight. The nitrogen contents and
the carbon-to-nitrogen ratios of the vari-
ous organisms are given in table 18.
Effect of adding
low-nitrogen materials
From this background some calcula-
tions follow which give the microbio-
logical basis for well-known reactions
observed when certain materials are
added to soil.
If 100 pounds of wood shavings con-
taining 35 per cent carbon and 0.2 per
cent nitrogen are added to soil, the fol-
lowing calculations indicate the results
of its complete decomposition by fungi:
100 pounds of shavings = 35 pounds
of carbon and 0.2 pound of nitrogen
35 pounds of carbon, 40 per cent as-
similated by fungi = 14 pounds of
carbon assimilated
Ratio of carbon to nitrogen in fungi
=10 to 1 == 1.4 pounds of nitrogen
assimilated.
The amount of nitrogen furnished by
the shavings was 0.2 pound and that
used by the fungi 1.4 pounds; therefore
1.2 pounds of nitrogen would have to be
supplied to the fungi for the decomposi-
tion. Thus the soil microorganisms
would be competing with the plant for
the available nitrogen in the soil. In most
cases the microorganisms are more suc-
cessful than crop plants in obtaining the
nitrogen needed.
Table 1 8. Average Nitrogen and Carbon Contents of Organisms
Fungi
Bacteria
Actinomycetes
Mature higher plants
Per cent of
carbon in
nutrients used
40
25
25
Nitrogen con-
tent of the cells,
in per cent of
dry wt.
5
10
8.5
1.5
Ratio of carbon
to nitrogen in
the cells
10 to 1
5 to 1
6 to 1
20 to 1
* Based on data by Waksman and Starkey (1931).
[242 1
This process explains the temporary
nitrogen deficiency noted in plants after
the application of wood shavings and
other materials low in nitrogen. Experi-
mental data of 0. A. Matkin (unpub-
lished) show that 1 bushel of sawdust
can completely tie up the available nitro-
gen for 6 weeks when % pound of hoof
and horn meal is added, and remove the
available nitrates for the same period
even with the addition of 3 pounds of
hoof and horn.
Assimilation of nitrogen by microor-
ganisms does not mean that nitrogen is
permanently tied up in microbial cells.
Microorganisms are relatively short-
lived (for example, bacterial cells may
live only 2 days, those of fungi several
weeks), and upon their death and de-
composition by other organisms the
nitrogen and other elements which were
assimilated are partially released.
The temporary nitrogen deficiency
caused by additions of low-nitrogen
materials can be overcome by the addi-
tion of inorganic nitrogen fertilizers or
by composting the organic materials
with nitrogen before planting. Compost-
ing enables the material to be decom-
posed and to reach a relatively stable
state before its use. Composted material
does not support the rapid growth of
organisms resulting in nitrogen competi-
tion. There are, however, numerous
disadvantages in its use (Sec. 6).
A very striking example of rapid mi-
crobial use of nitrogen occurs with the
addition of sugar to soil. Sugar has a
high carbon percentage, no nitrogen,
and is water-soluble. A small amount
added to soil high in available nitrogen
will so enhance microbial development
as to completely tie up the nitrogen in
less than 2 days. This phenomenon has
been used in the laboratory to reduce
the soluble nitrogen in pots of experi-
mental plants, with rapid and complete
results. Some growers have used it to
prevent soft growth of their plants in
recently fertilized soil when confronted
with an unexpected cloudy period. Most
reports, including those from Matkin,
agree that with organic materials con-
taining less than 1.5 to 2 per cent nitro-
gen a deficiency usually results upon
decomposition.
Effect of adding materials with
over 2 per cent nitrogen
Materials containing over 2 per cent
nitrogen supply more than is required
by the microorganisms. This excess ap-
pears as ammonium (later oxidized by
bacteria to nitrate under many condi-
tions) .
An example of a material with more
than 2 per cent nitrogen is dried blood
meal. If completely decomposed by
fungi, the following calculations would
apply :
100 pounds of dried blood
40 per cent carbon = 40 pounds of
carbon
13 per cent nitrogen = 13 pounds of
nitrogen
40 pounds of carbon, 40 per cent as-
similated by fungi = 16 pounds of
carbon assimilated.
Ratio of carbon to nitrogen for fungi
= 10 to 1 = 1.6 pounds of nitrogen
assimilated.
Nitrogen available for crop, 11.4
pounds.
The excess nitrogen would appear as
ammonium as the decomposition pro-
gressed. The ammonium, a waste product
in the nutrition of the fungi, then would
be available to higher plants. These
processes clarify the plant stimulation
that occurs when organic matter with
more than 2 per cent nitrogen is added
to soil.
Similar calculations could be made to
illustrate the results of the same decom-
positions by bacteria or actinomycetes.
Bacteria and actinomycetes assimilate
less carbon than fungi, but have higher
nitrogen requirements.
[243]
The cells of microorganisms contain
more than 2 per cent nitrogen and thus
when they die and are decomposed by
other organisms nitrogen becomes avail-
able.
Effect of Environmental Factors
Temperature
Since the availability of elements from
organic materials depends upon their
liberation by the activities of organisms,
any factor affecting the growth of soil
organisms will also affect the availability
of such plant nutrients. The effect of
temperature exemplifies this principle.
At optimum temperatures for soil organ-
isms, organic matter is broken down
most efficiently. The process, mentioned
earlier, of using sugar on soil to reduce
available nitrogen proceeds most rapidly
at the optimum temperatures for the
organisms involved. Many growers have
noted how much longer it takes organic
nitrogen to become available in winter
than in summer. Soil may also be stored
longer at lower temperatures before the
decomposition of organic materials re-
leases a toxic concentration of nitrogen
(Sec. 7).
Oxygen supply
The formation of peat, an important
constituent of the U. C.-type mixes, illus-
trates the effect of a lack of gaseous
oxygen on decomposition by organisms.
The saturation with water of the mate-
rial in peat bogs, and the resulting ex-
clusion of air, prevents the complete
oxidation of the organic matter. Aerobic
fungi and bacteria cannot function
under these conditions, and the decom-
position of organic matter is dependent
largely upon the activities of anaerobic
bacteria. These organisms can function
without oxygen from the air, but can
decompose only slight amounts of such
organic constituents as waxes and lignin,
while other constituents are broken
down very slowly. Peat is formed as the
result of the accumulation of resistant
plant residues over a long period of time
in an air-free habitat. Once formed, it
resists decomposition, even when ex-
posed to air. Hence, although it contains
only about 1 per cent nitrogen, it does
not cause a nitrogen deficiency. This is
one reason why it is a very important
constituent in the U. C.-type mixes. Red-
wood sawdust and shavings are better
for use in U. C.-type mixes than are
those from pine and fir, for the same
reason.
These examples illustrate the impor-
tance of soil organisms and the processes
they perform. By understanding that
any factor affecting growth of micro-
organisms affects plant growth, much
mystery in growing plants is explained.
TRANSFORMATION OF PLANT NUTRIENTS
BY MICROORGANISMS
Nitrogen
The primary source of soil nitrogen is
the atmosphere. The nitrogen in the air,
however, is in the form of an inert gas
which becomes available to green plants
only as it is changed into combined
forms by specific soil microorganisms or
chemical processes. Natural electrical
discharges add a negligible amount of
inorganic nitrogen compounds to soil.
The bulk of chemically combined nitro-
gen is produced artificially by commer-
cial fixation processes, generally produc-
ing ammonium or cyanamide. The main
natural means by which plants obtain
nitrogen from the atmosphere is as a
result of the activities of certain soil
microorganisms.
[244]
Denitrification
-^ Microorganisms
NITRATE NITROGEN] Higher p|anfs
NO,
available to plants
Nonsymbiotic and symbiotic
nitrogen-fixing bacteria
A
"t
Denitrification
Bacteria and fungi
Feed on
ORGANIC NITROGEN
in protein of cells of
plants and microorganisms; j plant material
not available to plants
ORGANIC NITROGEN
_^ in protein of cells
of animals;
not available to plants
/
Specific bacteria,
Nitrobacter spp.
Various organisms: fungi,
bacteria, actinomycetes
-->
NITRITE NITROGEN
NO 2
toxic to plants
Nitrosomonas spp.
Specific bacteria,
Bacteria >
11/
AMMONIUM NITROi
NH4
available to plants
Fig. 1 17. Schematic representation of the most important nitrogen transformations in soils.
Nitrogen-fixing bacteria
As seen in figure 117, atmospheric
nitrogen is fixed into microbial cell
material by free-living bacteria. This re-
action does not produce appreciable
amounts of nitrogen, especially in soils
with growing plants.
Symbiotic nitrogen-fixing bacteria,
which live in the root nodules of legumes,
cause the fixation of atmospheric nitro-
gen, which becomes available to their
host plant. Symbiotically fixed nitrogen
is a very important source of nitrogen,
but limited to the Leguminosae.
Ammonifiers and nitrifiers
Whatever the source, if the nitrogen
is tied up in organic compounds (plant
materials or animal materials) the ac-
tion of soil organisms is required to
convert it to ammonium or nitrate nitro-
gen before the plant can utilize it. Some
organisms first carry the reactions from
ammonium to nitrite, and then others
convert from nitrite to nitrate nitrogen.
Denitrification (reduction of nitrate to
nitrite and then to gaseous nitrogen)
can be performed by many organisms,
but is not important where soil is well
aerated.
The essentials of nitrogen conversion
in soils are summarized as shown below.
Organic nitrogen (unavailable to plants
except in the rare uptake of amino
acids) is broken down by various kinds
of organisms to produce ammonium.
Many common air-borne fungi, actino-
mycetes, and bacteria (including spore-
formers) are capable of causing this
conversion.
The steps from ammonium to nitrate,
on the contrary, are performed by
specific, non-spore-forming bacteria.
Organic nitrogen
(unavailable)
Type 1
organisms
Bacteria
Fungi
Actinomycetes
Ammonium
(available)
Type 2
organisms
Specific
bacteria
Nitrate
(available)
[245]
These bacteria are among the most sen-
sitive of soil organisms. Conditions and
treatments (heat, chemicals, pH, and so
on) readily withstood by the ammonify-
ing organisms cause injury or death to
the nitrifying bacteria.
The specificity and sensitivity of the
nitrifiers, as opposed to the abundant
types and hardiness of the ammonifying
organisms, account for the fact that am-
monium is produced under a much
broader range of conditions than is
nitrate. Conditions and treatments which
inhibit the nitrifiers often have little
effect on ammonium production. For
example, highly acid media inhibit nitri-
fication much more than ammonium
formation, as illustrated in the following
data from Section 7.
In a growing medium at pH 3.9 the
total ammonium and nitrate nitrogen
was 251 ppm, of which only 26 ppm was
in the nitrate form. However, at pH 5.9,
with a total of 505 ppm, 350 ppm ap-
peared in the nitrate form. Thus the
medium at pH 5.9 had about twice as
much total available nitrogen but nearly
fourteen times as much in the nitrate
form as in the medium at pH 3.9.
Low temperatures also reduce nitrifi-
cation much more than ammonification.
Under most environments some organ-
isms included in the ammonifying popu-
lation can grow at temperatures that
inhibit the specific bacteria concerned
with nitrification. In normal, untreated
field soil, however, the bulk of nitrogen
available to the plant appears in the
nitrate form. Ammonium formation
usually becomes a factor only after some
type of soil treatment, as is considered
later in this section.
Carbon
Carbon makes up an average of ap-
proximately 50 per cent of the dry
weight of all chemical elements in plant
and animal tissues. Carbon dioxide gas
ia the source of carbon for the growth of
green plants. Animals derive their car-
bon from plant materials. Thus, the
primary source of carbon for plant and
animal life is carbon dioxide gas.
Carbon dioxide is present in the at-
mosphere in a concentration of 0.03 per
cent, and about %5 of the total carbon
content of the atmosphere is consumed
each year by the plant world. This sup-
ply is never exhausted, however, largely
because it is constantly being replen-
ished by the microbial decomposition of
organic substances in the soil, but also
by means of plant and animal respira-
tion and industrial burning. When mi-
croorganisms completely decompose an
organic material, the carbon goes off as
carbon dioxide.
Because of the activities of soil mi-
crobes, the atmosphere of the soil con-
tains from 20 to 200 times as much
carbon dioxide as air. This high carbon
dioxide content of the soil results in the
formation of carbonic acid, which aids
in bringing insoluble elements such as
phosphorus into solution. The produc-
tion of carbon dioxide from soil is, in
fact, often used as a measure of the
activity of the soil microbial population.
The transformations of carbon are sum-
marized in figure 118.
Sulfur
Sulfur is another element essential to
plant growth that undergoes microbial
transformation. Sulfur reaches soil as
organic compounds (plant and animal
residues), elementary sulfur (fertilizers,
fungicides, soil amendments), or sul-
fates (fertilizers, amendments, irriga-
tion water) .
The transformation of sulfur-contain-
ing organic compounds resembles that
of nitrogen. Instead of ammonium
(NH4), hydrogen sulfide (H2S) is
formed, and through various reactions
sulfate (SO.,) is produced. Bacteria
known as "sulfur bacteria" are respon-
sible for the rapid conversion of ele-
mental sulfur to sulfuric acid.
[ 246 ]
/*
Atmospheric
Carbon Dioxide
co2
Photosynthesis
t
Respiration
Microbial
Decomposition
Microbial
Decomposition
Respiration
Fig. 1 18. The carbon cycle.
Plants
Organic
Compounds
Animals feeding
on plants
I
Animals
Organic
Compounds
j
This change (oxidation) not only
renders the sulfur available for plants
but makes the soil reaction more acid.
The reaction is made use of in reclaim-
ing alkali soils, to reduce certain plant
diseases such as potato scab, to increase
iron and phosphate availability, and to
make soil slightly acid or neutral for the
growth of certain plants. One pound of
soil sulfur when oxidized to sulfate by
organisms produces about 3 pounds of
sulfuric acid.
Phosphorus
Phosphorus, essential for plant growth,
is found in soil organic compounds or
as insoluble phosphates. Several bacteria
and fungi can liberate phosphorus from
organic compounds in an inorganic
form. Phosphorus is a constituent of mi-
crobial cells and, just as with nitrogen,
may be rendered temporarily unavail-
able to plants when materials low in
phosphorus are rapidly decomposed.
Insoluble phosphates are made avail-
able mainly by the indirect action of
microorganisms. Many of the organic
and inorganic acids produced by soil
microbes react with the insoluble phos-
phates to form soluble compounds. Ger-
retsen (1948) has shown that organisms
in the rhizosphere have considerable
solvent action on insoluble phosphates.
In the past this has been attributed to the
roots themselves.
Other Essential Elements
Other essential elements such as potas-
sium, calcium, magnesium, and iron are
affected either directly or indirectly by
soil microorganisms. When organic sub-
stances are decomposed by microbes
they release potassium, which is then
available to higher plants. Although
potassium is usually added to the soil
in a soluble form, organic acids from
microorganisms help liberate it when it
becomes fixed by the soil. Calcium, mag-
nesium, and iron are affected indirectly
by the actions of soil organisms, espe-
cially through acid production.
Many experimenters have shown that
soil organisms can affect manganese
nutrition of plants. Manganese-deficiencv
symptoms can result from the action of
certain microorganisms that render
[247]
manganese insoluble by oxidizing it.
Treatments which eliminate the man-
ganese-oxidizing organisms alleviate the
deficiency.
A similar situation was reported in
California in the little-leaf rosette disease
of peaches, attributable to zinc defi-
ciency. Ark (1937) found high bacterial
concentrations in the root zone of sus-
ceptible trees, but overcame the trouble
by applying zinc salts or by sterilizing
the soil.
Most elements essential to plant
growth are also required by soil organ-
isms. This direct competition, along with
indirect effects, such as release of acids,
so closely links the activities of these two
groups that any change in the microbial
population has an effect on plant nutri-
tion.
EFFECT OF SOIL TREATMENTS ON MICROORGANISMS
One of the important considerations
in the increasing use of soil treatments
by chemicals and steam is their effect on
the population of soil organisms, both
harmful and beneficial. When soil is
treated with the recommended chemicals
(Sec. 11) or steam (sees. 8 and 9) many
excellent results are achieved. Soil-borne
plant pathogens are controlled, weeds
and insects are eliminated, and very
marked plant-growth increases result
(fig. 119). Treatment of soils is neces-
sary because of these many advantages,
but the effect on beneficial soil organ-
isms may be disadvantageous.
decontamination Hazard
When soil is treated, the number of
soil microorganisms is greatly reduced
for the first few days; then it rises and
eventually exceeds that of untreated soil.
Let us consider what occurs when the
soil is treated, and disease organisms
gain access to this soil. The treatment
destroys a large part of the dense popu-
lation of soil microbes, and the first
organisms to return after treatment meet
no severe competition. Thus, if plant
pathogens are among the first to re-
colonize the soil, they develop rapidly,
.■:■■;:■ ,,;
Fig. 119. Increased growth of tobacco plants in chloropicrin-treated soil as compared to un-
treated soil (left).
[ 248 ]
Fig. 120. The effect of steaming field soil on plant growth and disease spread. A, Steamed
soil; excellent stand and growth. B, Nontreated soil; poorer stand and growth than in A.
C, Steamed soil with Rhizoctonia added at arrows, showing greater pre- and postemergence
damping-off than in nonsteamed soil. D, Nonsteamed soil with Rhizoctonia added at arrows.
and cause severe disease losses. It there-
fore is important to the grower that
pathogens do not gain entrance to
treated soil. Benches, flats, equipment,
seed, and the numerous other sources of
pathogen introduction (Sec. 3) become
Danger of Inadequate Treatment
One source of trouble is the use of
treatments which destroy a portion of
the soil population, but leave pathogens
unharmed. Severe losses often occur
after such treatments, because of the in-
potentially more dangerous when using crease of the surviving pathogens under
treated as compared with untreated soil.
The damping-off of seedlings in nur-
sery soils in California caused by the
soil fungus Rhizoctonia solani may be
cited as an example (Sec. 3). This path-
ogen can be effectively eliminated from
soil by any of several treatments. If,
however, the fungus then gets into this
treated soil, the resulting loss is much
more severe than that suffered in un-
treated soil (fig. 120).
the conditions of decreased competition.
The two most common ways of creating
the above condition are:
1. The use of fungicidal treatments at
lower than recommended rates.
2. The use of treatments that control
other pests or specific diseases and
may markedly decrease the soil popu-
lation, but not destroy certain plant
pathogens.
In both cases the loss results from the dis-
ruption of the balance in the soil popula-
[249]
tion and the shift to conditions favoring
the increase of a plant pathogen.
Examples of damage due to treatments
at too low a dosage are most often seen
with treatment-resistant pathogens such
as the soil fungus Verticillium albo-
atrum. V erticillium is relatively hard to
kill and therefore it is possible to apply
treatments which remove much of the
soil population, leaving V erticillium to
infect more severely. Where V erticillium,
Fusarium, or other more resistant fungi
are a problem it is dangerous to use less
than recommended dosages for their
control. Also, if treatments for control
of these diseases are done improperly or
incompletely, the same severe loss can
occur as from too low a dosage.
Examples of the second case are also
encountered where treatments for given
pests enhance the damage due to other
pathogens. Treatments used for the con-
trol of nematodes have sometimes re-
sulted in increased losses from Verticil-
Hum wilt. One experimental fungicide
recommended specifically for Rhizoc-
tonia control has been reported to con-
trol Rhizoctonia, but heavy losses due to
water molds, not important before treat-
ment, may then be sustained.
These examples are cited to illustrate
the role soil microorganisms play in
disease control, and the importance of
considering them in all control opera-
tions.
Increased Need for Sanitation
The proved advantages and wide-
spread use of soil treatments with the
resulting increased hazard and severe
effects of recontamination, point to the
need of a more thorough knowledge of
the sources and means of combating
pathogen introduction. The most impor-
tant means of eliminating sources of con-
tamination is a vigorous and constant
program of sanitation. To reap the full
benefits of soil treatment the grower
must ever be on guard to protect the
treated soil. Every operation must be
checked for the possible introduction of
disease material (see "A Nursery Sanita-
tion Code" in Sec. 1). The chain of suc-
cessful growing, though containing
strong links of adequate nutrition,
disease-free soil, and clean stock, can
easily break if a weak link, such as the
presence of pathogens on flats or
benches, exists.
The alert grower can more effectively
combat recontamination if he under-
stands something about the sources of
disease organisms and the practices
which introduce them into soil. The two
main channels of introducing pathogens
into pathogen-free nursery soil are
planting stock and infested soil or plant
particles which may come into contact
with the clean soil in many ways. The
most important plant pathogens causing
damping-off, root rots, and related
diseases are not air-borne, but must de-
pend upon the mechanical transfer of
infested soil or water and infected plant
tissue for their spread (Sec. 3) . This fact
enables the alert grower to reduce or
eliminate the transfer of infested mate-
rial by careful practices.
CONTROLLED COLONIZATION: A FUTURE STEP
To Retard Pathogens
Since soil treatment has proved so
advantageous and is so widely used, and
since contamination of treated soil may
be severe, there is need for a method of
protecting treated soil from introduced
disease organisms. In an effort to meet
this need, studies were conducted by the
author, using organisms antagonistic to
plant pathogens but without adverse
effect on plants. The purpose of report-
ing this work is not to make any recom-
mendations at this time, but to provide
advance information on some steps be-
I 250 1
ing taken toward a future solution of
soil-disease problems.
The retardant organisms, singly or in
groups, are added to soil immediately
after treatment. Since they are the first
to return, they make rapid growth, just
as would pathogens if they were the first
organisms returning after treatment.
These beneficial or pathogen-retarding
organisms colonize the soil and protect
it from recontamination. They act either
as antibiotic producers or as parasites or
competitors of pathogens or in various
combinations of these types. The con-
tinual production of antibiotics in the
soil by organisms appears more effective
than the addition of antibiotics alone,
since these chemicals break down
rapidly. The effect of several different
organisms in restricting the spread or
completely stopping damping-off due to
Rhizoctonia solani is illustrated in figures
121 and 122. A retardant organism was
added to flats of steamed U. C.-type mix
at the time of seeding. The flats were
also inoculated with Rhizoctonia in
heavy enough concentration to cause
eventual 100 per cent loss in flats not
protected with retardant organisms.
Complications
The results are very encouraging, but
some of the complications should be dis-
cussed. The Rhizoctonia-r etar ding effect
appears to last for the entire susceptible
seedling stage with some organisms, but
is only temporary with others. The re-
tarding effect of Myrothecium (a com-
mon soil fungus) diminished after a
month in flats with growing plants. In-
creased concentrations of Myrothecium
high enough to inhibit Rhizoctonia for
longer periods stunted the pepper seed-
lings. Both this stunting effect (fig. 123)
and the Rhizoctonia-retarding effect
could be enhanced by the addition of
various organic amendments. Since
Myrothecium is a rapid cellulose decom-
poser, materials high in cellulose gave
the greatest effect. This case serves to
Fig. 121. The effect of adding Rhizoctonia
with and without a retardant (Myrothecium) to
flats of a steamed U. C.-type mix planted to
peppers. A, (upper right) Rhizoctonia plus My-
rothecium added at this point; damping-off
prevented. B, (lower left) Rhizoctonia added
at this point; damping-off severe and continu-
ing.
illustrate the sequence of organisms in
soil resulting from the addition of or-
ganic matter. When cellulose-rich mate-
rial was first added, the Myrothecium
population increased rapidly, with re-
sulting retarding effect on Rhizoctonia.
As the cellulose became decomposed the
population shifted, and with other or-
ganisms becoming dominant the retard-
ing effect of Myrothecium on Rhizoc-
tonia diminished.
The soil pH has a marked influence on
the organisms used in controlled coloni-
zation. In the acid range, fungi such as
species of Penicillium and Trichoderma
are most effective, while, as the reaction
approaches neutrality, species of the
genus Streptomyces become more prom-
ising.
Competition escape accounts for one
of the difficulties encountered in the con-
trolled colonization work. A soil may be
colonized with a Rhizoctonia-retarding
organism to the extent that growth of
Rhizoctonia is completely restricted. If
this same soil contains growing plants,
Rhizoctonia may spread from plant to
[251]
Fig. 122. Protection from Rhizoctonia damping-off achieved by the addition of a retarding
organism to flats of a steamed U. C.-type mix planted to peppers. A, Control flat; no retardant
or Rhizoctonia added. B, Trichoderma sp. added as a retardant to the whole flat, and Rhizoctonia
added at arrow; resulted in complete protection comparable to control flat. C, Penicillium sp.
added as a retardant to the whole flat, and Rhizoctonia added at arrow; resulted in a small
area of preemergence damping-off, but no postemergence damping-off. D, Rhizoctonia alone
added at arrow; resulted in complete loss.
plant above the soil surface. Thus, under
conditions of plant crowding and high
humidity, Rhizoctonia may escape the
retarding effect of the soil flora.
The above complications do not mean
that it will not prove feasible to use con-
trolled colonization to protect against
disease loss, but indicate the need for
further study and knowledge of soil
microorganisms in relation to plants.
Prerequisites for the program
The entire concept of biological con-
trol of soil-borne plant pathogens shows
increasing promise, and the nursery in-
dustry is unique in having available all
the features requisite for a successful
program using beneficial organisms.
Before the addition of organisms to
soil can be effective in protecting the soil
from subsequent contamination by path-
ogens,, most of the existing soil micro-
flora must be destroyed or the existing
organism balance changed in some other
way. This is already accomplished in
most nurseries by either steam or chemi-
cal soil treatment.
Consistent protection by beneficial
organisms is also dependent upon a
uniform soil. This is most satisfactorily
obtained by the use of a U. C.-type soil
mix, which can be accurately duplicated.
Finally, the controlled and stable con-
ditions of nursery growing further add
feasibility to obtaining positive results
with biological control. California nur-
[ 252 ]
sery operations so closely parallel the
laboratory conditions used in these
studies that results in protecting soil
against pathogens, such as those illus-
trated above, appear to be entirely pos-
sible. No major modifications of the
ultimate techniques developed in the re-
search laboratory should be necessary
for commercial application.
Untreated soil contains such an abun-
dance of life that little is gained by
adding organisms without some type of
treatment to overcome the natural
biological buffering capacity of the soil.
This can be accomplished by treatment
to alter the soil population, or by sup-
plying a specific nutrient substrate to
make a favorable environment for the
desired organisms. Other environmental
factors such as pH, temperature, and
moisture can also influence the popula-
tion and can be controlled. It is impor-
tant that the grower realize that he
cannot simply add an organism to the
soil and expect it to have some desirable
effect.
To Improve Nitrogen Nutrition
In addition to the effect on disease,
removal of beneficial soil organisms can
adversely affect the nitrogen nutrition of
plants. Two points are considered:
1. An initially low level of available
nitrogen after treatment.
2. The bulk of available nitrogen after
treatment appears in the ammonium
form. In general, plants continually sup-
plied with ammonium synthesize organic
nitrogen rapidly and thus tend to deplete
their supply of sugars and starch (Sec.
7). An undesirable condition of carbo-
hydrate deficiency may result in softer
and more succulent plants, as in the case
of snapdragon seedlings. Often plants
in this condition cannot survive trans-
planting. Nitrate is absorbed and used
Fig. 123. The effect of amendments in increasing both the retarding effect on Rhizoctonia and
the stunting of plants when added with Myrothecium to flats of a steamed U. C.-type mix planted
to peppers. Left, sterilized wheat straw added to upper half, no amendment to lower half of
flat. Note greater restriction of Rhizoctonia damping-off with the wheat straw amendment. Right,
sterilized pepper seeds added to upper half, no amendment to lower half of flat. The three
representative seedlings on each card show the greater stunting of pepper seedlings when sterile
pepper seeds are added.
[253]
comparatively more slowly, and plants
supplied this form of nitrogen usually
form more lignin and cellulose, the
major constituents of the mechanical
tissues of plants. A few plants apparently
require at least part of their nitrogen in
the nitrate form for best growth. Am-
monium can also be toxic if high enough
concentrations are reached (Sec. 7).
As explained earlier, organisms are
needed to convert unavailable organic
nitrogen into an available form. The
initial reduction in all organisms im-
mediately after treatment accounts for
the initial lag in available nitrogen from
organic sources. A partial alleviation of
this low initial nitrogen level could be
achieved by the introduction of organ-
isms especially efficient in converting un-
available organic nitrogen into available
forms. Experiments with several soil
fungi have shown this approach to be
feasible. The use of nitrate starter solu-
tions is also helpful (Sec. 7).
Introducing nitrifiers
After steaming, the predominant
available nitrogen is in the ammonium
form, owing to the abundance and re-
sistance of type-1 organisms as compared
with those of type 2 (p. 245). Further-
more, the type-1 organisms include
many common air-borne fungi, actino-
mycetes, and bacteria. These organisms
colonize treated soil with comparative
rapidity and some of the spore-forming
bacteria survive most treatments. In con-
trast, the type-2 or nitrifying organisms
are readily killed by most treatments and
are much fewer in species and numbers.
Thus, the nature of the organisms in-
volved explains the ammonium accumu-
lation, and also indicates a method of
carrying the reaction on to the forma-
tion of nitrate nitrogen by adding the
appropriate organisms to soil. This has
been accomplished in the University
laboratories in Los Angeles by adding
to the steamed mix a water suspension of
soil containing nitrifying organisms. As
discussed in Section 7, in 21 days the
nitrate nitrogen in one series with in-
oculated soil averaged 101 ppm com-
pared to 8 ppm in soil not inoculated
with nitrifying organisms. To be com-
pletely practical for all cases the time
required to reach the 21-day level should
be reduced, but these tests show the po-
tential value of controlling soil nitrogen
by adding certain organisms.
A Possible Future Program
A future program for a grower of
plants in containers may be envisioned
from these facts. Flats, pots, and other
containers filled with a U. C.-type soil
mix are treated with steam or chemicals
to remove all organisms, and then a
suspension of organisms is sprayed on
the flats before planting. This suspension
would include organisms capable of sup-
pressing accidentally introduced patho-
gens. Also included would be organisms
which would promote the early produc-
tion of nitrate nitrogen. This program
would greatly reduce or eliminate soil-
borne disease problems and would give
plants grown in this way a measure of
protection even if set out for growing in
untreated field soil. Plant nutrition when
organic nitrogen is used would be
greatly improved. With all the special
features of nursery growing in a U. C.-
type soil mix, this program is a definite
possibility.
[254]
SECTION
Importance of Variation
and Quantity of Pathogens
Richard D. Durbin
The variability of plant pathogens
The inoculum potential
Infected seed and stock
Longevity in soil
Mixed infections
Obligation of the nursery
rowers often ask, "Since rhizoc is
already present in my soil, what dif-
ference does it make if I introduce more
of it?" It is commonly assumed that be-
cause a fungus is present in the soil, the
inadvertent addition of more of it with
infected nursery stock, seed, bulbs, or in-
fested soil will make little or no dif-
ference in crop losses. This mistaken rea-
soning can have serious consequences;
it may lead to loss of the given crop and
infestation of the field, ruining it for cer-
tain crops.
THE VARIABILITY OF PLANT PATHOGENS
The variability of living organisms is
quite generally accepted. Every indi-
vidual in a given species is different in
many respects from all the rest, yet
shares certain common characters with
the other members of the species. Thus
we say that plants and animals having
the same scientific or common name are
similar but not identical. All humans
are classified as Homo sapiens, although
we have only to look around to see that
each is unique in some respect. In flower-
ing plants man has taken advantage of
some of the apparent differences within
crop species to develop varieties which
are outstanding in yield, quality, or
adaptability to certain environments.
Lower plants, such as fungi and bac-
teria, also exhibit this characteristic
variation, but it is not so evident because
of their small size. Variation in these
microorganisms may be evident in the
things they are able to do, that is, in
their physiological activities; for in-
[255]
stance, they may produce more or a
slightly different form of a substance
such as penicillin or streptomycin. While
this fact has been of great benefit to in-
dustry, it has seriously complicated the
prevention of diseases in plants and
animals.
Since the ability to produce plant dis-
ease involves the interaction of complex
physiological systems of pathogen and
host, it is not surprising that one also
finds variation here. The extensive varia-
tion among crop plants is not considered
in this section, but some mention of
parasite variation is pertinent. This sub-
ject is of concern to both grower and
pathologist.
Host Range and Virulence
Fungi
The fungus Rhizoctonia solani con-
tains individuals or strains which may
vary in host range, pathogenicity on
any one host, and response to the en-
vironment. Each strain is able to attack
a given group of plants, with the patho-
genicity of many strains overlapping
on a single host. One strain may be
strongly virulent to pepper but unable
to attack Tagetes, whereas another may
attack Tagetes vigorously; some strains
from tomato are virulent to bean while
others are not. Many such examples
exist. On any particular host plant the
disease produced may vary from stunt-
ing to complete loss from damping-off,
according to the strain involved.
In one test on variability in patho-
genicity, eleven isolates of Rhizoctonia
solani were compared in virulence to
pepper seedlings; figure 124 shows some
typical results. Although pathogenic to
the source host in each case, many of
the isolates were not pathogenic to
pepper, while others were more damag-
ing than was one originally from pepper.
These differences in virulence among
the isolates exemplify the danger of in-
troducing additional Rhizoctonia into an
already infested soil. Why take the
chance?
Some strains of Rhizoctonia solani are
almost saprophytic and cause little plant
damage, such as those commonly pro-
ducing black sclerotia ("the dirt that
won't wash off") on potato tubers. Dif-
ferent strains are now known to cause a
serious potato stem rot, although for
many years they were considered to be
the same as the tuber-attacking forms.
Tubers were even treated with fungicides
to eradicate the sclerotia in the hope of
stopping the stem rot, until it was dis-
covered that the diseases were different.
Still other strains of R. solani are re-
stricted to the above-ground environ-
ment, and cause foliar blights of various
crops in the southeast United States. In
southern California we are most familiar
with strains causing root rots and damp-
ing-off of nursery crops.
Stephen Wilhelm1 has found that
Verticillium albo-atrum includes forms
varying from those apparently unable to
invade the host, through those which
may invade without producing the dis-
ease, to those which invade and produce
varying degrees of disease on a given
host. Some forms that do little harm on
one host may be severe on another. Thus,
among isolates pathogenic to stock some
are nonpathogenic on tomato, others in-
vade tomato roots but cause no above-
ground disease symptoms, while still
other isolates are severely pathogenic to
tomato. Furthermore, Wilhelm and
Raabe (1956) have recently found a
strain of Verticillium albo-atrum that
produced wilt on the Manetti rose root-
stock, formerly resistant to known strains
of this fungus.
The genus Fusarium includes types
which live saprophytically, or cause
cortical stem and root rot or vascular
wilts. F. oxysporum includes sapro-
phytes as well as about twenty-five
named forms that are highly specific in
1 Department of Plant Pathology, University
of California, Berkeley; unpublished data.
[ 256 ]
Fig. 124. Effect of several isolates of Rhizoctonia solani on pepper seedlings. Seeds were sown
in treated soil and immediately inoculated at the lower end with equal amounts of the fungus
isolate. The area inside the white line is the zone of preemergence damping-off. Photos taken
18 days after planting. Left to right, top row: uninoculated; inoculated with a gladiolus isolate
(isolates from tung, soybean, cotton, Dieffenbachia, and alfalfa responded in the same way);
inoculated with a mild isolate from pepper. Left to right, bottom row: inoculated with a poin-
settia isolate; inoculated with an isolate from morning-glory (an isolate from lima bean re-
sponded in the same way); inoculated with a virulent isolate from pepper. The mild pepper
isolate caused post- but no preemergence damping-off, while the poinsettia isolate caused
pre- but almost no postemergence damping-off. The virulent pepper isolate caused both the pre-
and postemergence phases.
their ability to invade the vascular sys-
tem of plants. These forms are so spe-
cific that one of them will attack only
certain varieties of a given crop species,
a fact utilized in controlling them
through resistance. Thus, the form which
attacks aster is limited to that crop and
to certain varieties of it as well. Oc-
casionally a form appears that is able
to attack a crop variety (for example, of
tomato or pea) previously resistant to
the Fusarium wilt. In such cases this
may account for the apparent breakdown
of resistance, because in reality two dif-
ferent diseases are present. As in Rhizoc-
tonia, isolates of any one of these forms
may vary widely in the severity of dis-
ease they produce in a given susceptible
[257]
host variety. When a grower is indif-
ferent about introducing a Fusarium
wilt to his fields, he is ignoring the dis-
ease potentialities. For example, he may
not presently be raising asters and thus
be unconcerned about the dumping of
infested aster refuse or soil on his land.
Many years later he or someone else may
wish to plant asters in these fields, and
find that by the second year of the at-
tempt, the residual fungus has built up
and increased disease losses to a ruinous
extent.
Some growers assume that all water
molds are alike and that they occur
everywhere. However, some strains of
Pythium debaryanum are said to induce
100 per cent root rot of spruce seedlings,
while other strains under the same en-
vironmental conditions are purely sapro-
phytic. Roth and Riker (1943) found
that the damping-off of red pine varied
from 36 to 87 per cent under a given en-
vironment, again according to the strain
of the fungus used. It is now clear that
the worst disease problem of both
heather and avocado in California is
root rot caused by Phytophthora cin-
namomi. Although water molds as a
group may be generally distributed, this
one is not widespread in California even
yet, and those plantings suffering from
it usually can trace their infestation back
to the nursery source of the stock. There
is also evidence for some biological spe-
cialization within species of this genus.
According to Tucker (1931), Phytoph-
thora capsici and P. parasitica f. nico-
tianae are the only Phytophthora species
attacking pepper and tobacco, respec-
tively. #
Thielaviopsis basicola commonly
causes black root rot, stem decay, or
graft failure on ornamentals; it has a
host range of over 120 species in 30
families. It is known to be comprised of
races which cause varying amounts of
disease on some crops while on other
crops they may not be pathogenic at all.
Isolates from poinsettia, Primula ob-
conica, cyclamen, and tobacco, for ex-
ample, were reported in some inocula-
tion experiments as most pathogenic to
the host from which they were originally
isolated, while the reciprocal inocula-
tions yielded less, or in some cases no
disease. In other experiments isolates
from tobacco were more virulent on
Primula, but less virulent on cotton
seedlings than isolates from Primula
itself.
Bacteria
Variability in virulence has also been
noted in the bacterial pathogens that
cause fire blight and bacterial fasciation.
Crown gall has been shown to have
some degree of host specialization. Iso-
lates from marguerite daisy will produce
medium-size galls on tomato and rasp-
berry, but rarely do so on apple. Rasp-
berry and probably loganberry isolates
are pathogenic to tomato and apple but
not to marguerite, while some isolates
from apple do not seem to be pathogenic
to other hosts.
Nematodes
There are also host-restricted races in
plant-parasitic nematodes. In the stem or
bulb nematode, Ditylenchus dipsaci,
some of the "races" are comparatively
unspecialized and are parasitic on a
wide range of hosts; other "races" are
more specialized and able to attack only
a few hosts, while still others may sur-
vive only on one or two hosts. The
"races" attacking hyacinth and narcissus
bulbs fall into this last category. Ap-
parently nematodes attacking narcissus
cannot attack hyacinth, although they
may attack onions. Recent work has
shown that some of these "races" are
actually distinct nematodes (species).
This situation further illustrates the
danger in assuming that two pathogens
are identical because they are presently
called by the same name.
In what is generally called "the root-
knot disease," as though caused by a
[ 258 ]
single nematode species, it is now recog-
nized that several are actually involved,
and that they differ in host range. Shalil
peach rootstock in some areas has some-
times "lost resistance" to the nematode
when attacked by a different population
of what was then considered as one
species. Now we know that there are
three species of root-knot nematode com-
monly found in California, only one of
which attacks Shalil rootstock. Popula-
tions from Philodendron sp. are able to
multiply on Persian clover, but nema-
todes from Pothos aureus are not. Ac-
cording to the species or race of the
nematode present, some plants are at-
tacked in one locale but not in others. It
has even been suggested that populations
of root-knot nematode can be identified
on the basis of whether or not they attack
peanuts, pepper, watermelon, and Lyco-
persicon peruvianum, and by the reaction
of snapdragons to them.
Environmental Response
Not only may different strains of a
given microorganism exhibit differences
in respect to host range and severity of
attack, but they may exhibit differences
in response to physical and physiological
factors of the environment. In industry
this characteristic of physiological vari-
ation has been utilized to obtain strains
which are more efficient in doing specific
jobs, such as antibiotic production,
alcoholic fermentations, and production
of dairy goods, as well as an array of
many organic compounds.
Comparatively little is known about
the interactions of parasitic organisms
with other soil microorganisms and with
the host, and of the effects of fungicides,
soil atmosphere, light, nutrient or vita-
min deficiencies, or root secretions upon
them. Our knowledge in this field, how-
ever, is rapidly expanding.
Temperature relations
It has been reported that strains of
Rhizoctonia vary in temperature re-
quirements for disease production. The
optimum temperature may vary from
59° to 95° F. When two strains which
differ in their response to temperature
exist together in the soil, disease will
occur over a wider soil-temperature
range than if either is present alone.
Soil depth and carbon
dioxide content
Work in progress by the author in-
dicates that strains of Rhizoctonia solani
differ widely in their tolerance to the
concentrations of carbon dioxide found
in the soil. The fast-growing aerial iso-
lates are relatively intolerant of carbon
dioxide and therefore probably are
unable to compete successfully with
other organisms underground, where the
carbon dioxide often is 100 times the
atmospheric concentrations. Isolates
found at or near the soil surface are
more tolerant than aerial strains, but are
not as tolerant as some found attacking
roots 3 to 18 inches below the surface.
This subterranean type is thus able to
escape competition with organisms
found at the soil surface. This type has
become increasingly common in south-
ern California in recent years, perhaps
being spread with planting stock. These
relatively tolerant strains can more
easily grow in soils which have poor
aeration, as well as at greater depths in
the soil, andean thus parasitize roots that
might otherwise escape infection.
Growers can with safety only assume
that two organisms will prove different
in disease potentialities in the field, re-
gardless of similarity of names applied
to them or to the diseases they cause
(fig. 124). Evaluation of differences in
their disease potential in advance, like
the determination of their proper name,
is a specialist's job. From the growers'
standpoint each strain of a fungus should
be considered as causing a distinct dis-
ease, in that the introduction of a new
and different strain may increase disease
losses.
[259]
THE INOCULUM POTENTIAL
Even if the strains of a pathogen in-
troduced into the soil were the same as
those already present, it would still be
unwise knowingly to carry in more of
them with infested planting stock. Such
a practice usually builds up the amount
of the organism (inoculum potential) in
the soil, and would also distribute it
more uniformly through the field. The
inoculum potential is important, because
the disease symptoms which we see are
often the result of not one but many
attacks on the plant by the parasite.
Naturally, the more places the roots are
injured the more will be the loss of
normal root functions. Usually a higher
inoculum potential increases the inci-
dence and severity of the disease.
If a soil is only slightly infested with
the aster-wilt Fusarium, there usually
will be only a little disease if the soil
temperature remains below 60° F, but at
75° to 80° the losses will be severe. In
heavily infested soil, severe losses will
occur even below 60°. Thus, in a lightly
infested soil a grower can usually escape
severe losses in coastal California, but if
he builds up the inoculum he will be
unable to produce a crop in any season.
It has also been found that if a soil is
heavily infested with Rhizoctonia solani,
it is not possible to control damping-off
by the dilute formaldehyde soil treat-
ment method (Sec. 11), or by coating
the seed with protective fungicides;
either method is fairly effective in lightly
infested soil.
INFECTED SEED AND STOCK
Another point to be considered is that
a given strain of a fungus introduced on
or in the planting materials may cause
greater and more rapid disease losses
than a more virulent one in the soil. Be-
cause the fungus is already in the tissue,
or is so situated as to infect the host
quickly, the rapidity and severity of loss
may be more or less independent of the
amount of the organism present in the
soil.
It has been stated that plant materials
have been the source of some 90 per cent
of the plant diseases and insect pests
which have come to us from other
countries. At least fourteen pathogens are
carried by tomato seed; fourteen by iris
rhizomes; and eight by pepper seed.
It is very often true that the strains
of an organism carried with the seed-
ling or on the seed, bulbs, root divisions,
or other plant parts are particularly
virulent to it. Those strains best able to
attack the host do so, and build up a
high inoculum potential, and are there-
fore most likely to be carried over with
the stock. For example, the Rhizoctonia
strains stimulated to high activity in
pepper-seed fields, because of the pres-
ence of this host, are also most likely to
cause rot of the fruits in contact with
the soil there. Such fruit decay leads to
infection of the seed. The end result is,
then, that pepper seed often carries
strains of R. solani highly virulent to
pepper, and that, when these seeds are
planted, the strains are established in the
seedbed and new planting. One of the
most dangerous features of the transmis-
sion of organisms with seed or vegetative
parts is that the constant association of
the virulent strains of a pathogen and its
host is thus assured. Some organisms
such as the oak root fungus, Armillaria
mellea, cannot easily attack vigorous
growing plants directly from the soil.
r 260 i
They can do so, however, by means of
rootlike masses of mycelium (rhizo-
morphs) that grow out from a previously
infected plant part. In this case the intro-
duction of infected plants may provide
an especially effective center for the
spread of the fungus. Many other fungi
undoubtedly are in the same way pro-
vided with an effective focus for spread
in a planting. Using infected stock may
more than nullify any benefit gained
from soil treatment. For these reasons the
operation of an isolation house, through
which all new plant material passes be-
fore being planted in production areas,
is a sound idea (Sec. 13).
LONGEVITY IN SOIL
Many of these organisms are able to
survive indefinitely in the soil. There-
fore, introductions made today may not
be evident until many years later when
a proper host plant is cultivated. An
example of this is afforded in the
branched broomrape, Orobanche ra-
mosa, a higher plant parasitic on roots,
which appears to have been introduced
into Alameda County, California, on
nursery stock, a nonhost. Subsequent
cultivation of a host, tomato, on the
surrounding land has given rise to the
disease which in recent years has
reached serious proportions. This type
of situation can be avoided if the nur-
series steam the soil in which their stock
is grown.
Bacterial blight of stock carries over
for 1 year in the soil and bacterial stem
rot of geranium for about 3 months.
Organisms of this type do not persist in
the soil for long periods in the absence
of their hosts because they apparently
are unable to compete successfully with
other soil organisms. On the other hand,
Rhizoctonia, water molds, nematodes,
Verticillium, and wilt fusaria can exist
for many years saprophytically, on weed
hosts, or as resistant structures in the
soil. These facts must be taken into con-
sideration when evaluating disease-con-
trol programs, and growers should be
aware of the far-reaching dangers in-
volved when dealing with pathogens
capable of existing many years in soil.
MIXED INFECTIONS
In some instances disease is the result
of attack of not one, but two or more
organisms. In these cases the losses may
be greater than the injuries from each
working alone. In Fusarium wilt of cot-
ton, the association of the sting nema-
tode, Belonolaimus gracilis, with the
fungus will cause losses from wilt even
in supposedly resistant cotton varieties.
In the absence of the nematode, the
fungus is able to cause much less disease
on susceptible varieties and does not
damage resistant varieties at all. A
similar situation prevails in the inci-
dence of the tobacco black shank disease
caused by Phytophthora parasitica f.
nicotianae in association with root-knot
nematode. If growers introduce either
the nematode or the fungus in a field in
which the other part of the complex is
present, increased disease results. This
places an added responsibility on the
grower: to avoid introducing into his
growing areas a pathogen that may prove
to be an aggravating agency of a dis-
ease complex.
[261]
OBLIGATION OF THE NURSERY
It is always potentially dangerous,
and often an immediate risk, to intro-
duce a plant pathogen into a nursery or
field regardless of whether it is believed
to be present there already. It is probable
that the greater knowledge of tomorrow
will show that we have suffered grave
disease losses in our crops because of
today's thoughtless spread of organisms
believed to be "already present". There-
fore, the nurseryman has a special
obligation to produce stock free of dis-
ease organisms, and to sell only those
planting media (soil, leaf mold, manure)
that are also free of such pathogens. To
answer the initial question: There is no
such thing as a safe soil-infesting disease
organism !
[262]
SECTION
Grower Experience
with the U. C. System
R. H. Sciaroni
J. W. Huffman
Bedding plants
Vegetable plants
Pot and foliage plants
Can-grown woody plants
Bench and bed crops
Cymbidiums in beds
Landscape application of the U.C. system
General experience
HE implications and explanations of
the U. C. system have been presented in
preceding sections, and its application
and mechanization (Sec. 17) in several
types of California nurseries remain to
be reported. To illustrate how the sys-
tem is being adapted to varying condi-
tions, this section describes the expe-
riences and practices of twelve growers
of bedding plants, pot plants, foliage
plants, vegetable transplants for field use,
benched flower crops, cymbidiums, and
can-grown woody stock in five counties.
These changes have been slow to come
about, and were in the majority of nur-
series brought about only when tradition
and seemingly standardized practices
were broken. Those who changed to the
U. C. system have found that the tech-
nical assistance of a well-trained person
has reduced errors and eased the transi-
tion.
Numerous crops (snapdragon, carna-
tion, stock, calla, delphinium, Esther
Read and Majestic daisies, violet, gladi-
olus) were being successfully grown in
coastal southern and central California
fields of the same fine sandy soil that is
used in the mix. This gave additional
confidence in the U. C. system and
offered the possibility of transferring the
benefits of this soil to pot plant and
bench culture.
The transition began in commercial
nurseries in southern California in 1943,
but became general after 1950. In the
San Francisco Bay area apparently no
establishments used the U. C. system
[263]
prior to 1953; instead they employed the
native clay loam soils. One large green-
house establishment in central California
selected the location of its new range in
southern California on the basis of the
presence of the customary clay soil,
ignoring areas of the fine sand. This
range is now hauling in for its green-
house benches the soil that had earlier
been rejected.
BEDDING PLANTS
According to Mr. Jack L. Mather,
Manager of the former Bedding Plant
Advisory Board, California State De-
partment of Agriculture, about 80 per
cent of the bedding-plant growers in
southern California were using some
type of light soil mix in 1952-53. By
contrast, many growers in central Cali-
fornia are still using clay soils.
Nursery A . . .
is a small, well-established bedding-plant
concern in central California. This was
purchased by a young man with little
prior growing experience, although he
had sold retail stock. He was told by the
people from whom he purchased the
nursery and by other local growers that
some crops (alyssum, phlox, verbena,
peppers, and eggplant) could not be
grown in that climate. Because farm ad-
visors and agricultural inspectors em-
phasized the importance of producing
healthy stock, he fumigated his soil with
methyl bromide to rid it of disease
organisms and weeds. Because plant
growth was still poor, he sought further
assistance, learning that the nutritional
and salinity levels of manures and leaf
mold varied widely and were therefore
unreliable. He adopted a U. C.-type soil
mix, and has since been able to grow
crops very successfully, including those
which could not previously be produced.
II i^ intelligent and practical approach,
coupled with the use of the soil mixes
and of disease control, have produced
outstanding results.
Nursery B . . .
is a large establishment in southern
California thai produces flatted stock
for field planting by vegetable and cut-
flower growers and seedsmen, as well as
for retail sale. Several variations of the
U. C. system have been used since the
nursery was started in 1944. The soil has
consistently been steamed, and healthy
planting stock or heat-treated seed used.
Weeding of flats has been eliminated,
this benefit alone almost paying for the
cost of steaming. The nursery is fully
mechanized and, therefore, uses a mini-
mum labor force.
During a period when only peppers
were grown, seed was machine-sown in
flats which were stacked until germina-
tion had occurred. This saved about 10
to 14 days of growing time in the glass-
house, and an additional 10 to 14 days
were saved because the seedlings were
not set back by transplanting.
Because of the large variety of crops
presently grown, seedlings are trans-
planted from seed flats rather than the
seed sown in place.
This successful nursery is probably
the oldest user of the U. C. system. Be-
cause damping-off has never been a prob-
lem here, specialist growers have exten-
sively used their services for starting
plants.
Nursery C . . .
is a large southern California bedding
and vegetable plant producer. In 1948
the grower was attempting to maintain
many different compost soil mixes to suit
the supposed needs of the many dif-
ferent varieties of plants he was growing.
He had, for example, a petunia mix,
tomato mix, pansy mix, and others. His
stock piles were large and scattered,
r 264 ]
making the job of mixing difficult and
expensive.
Soil sterilization was not practiced
because these organic mixes broke down
when they were steamed and released
toxic amounts of soluble salts. Losses
from soil-borne diseases were stagger-
ing, the only control practice being that
of reduced watering.
A light soil mix seemed out of the
question, for it was thought to be costly
and inconvenient because of the neces-
sity of soil hauling. Most important of
all it was contrary to the generally ac-
cepted beliefs that had been followed in
40 years of nursery business.
In 1949. economic factors led to a
break in the tradition, and the conver-
sion to a L. C.-type soil mix got under
way. A small concrete mixer was used
for the first trials. Results were so out-
standing that a large concrete transit
mixer was purchased, and mechaniza-
tion was begun. The soil storage area
has been reduced from IV2 or 2 acres to
about 1 -3 acre. Two or three men are now
preparing as many as 2,000 flats per
day, a job that formerly required eight
or ten men. Soil-borne diseases, except
for an occasional chance recontamina-
tion, are unknown. X\ eeding has been
eliminated. All jobs have been standard-
ized and are well performed with semi-
skilled labor under intelligent super-
vision.
This nursery is now a leader in
mechanization and one of the strongest
advocates of the L. C.-type soil mixes.
The owner often states. "Each step leads
to the next, and rapidly pays for itself:
the only barrier to the light soil system
is tradition."
VEGETABLE PLANTS
A large volume of celery seedlings is
grown under glass in southern California
for field planting in areas where mosaic
is controlled by a celery-free period.
Pepper, eggplant, and tomato are also
started under glass for special purposes,
sometimes in large volume.
Nursery D . . .
is a large producer of celery seedlings in
Los Angeles County. Tests were con-
ducted by the Agricultural Extension
Service in this nursery in 1952-53, com-
paring a treated L. C.-type soil mix with
their conventional untreated composted
soil.
The compost consisted of % decom-
posed manure, ^ black peat, and 1a a
soil-sand blend, and had been composted
for a year or more. Decomposition was
not uniform because of differences in
temperature, moisture, amount of straw
contained in the manure, and other fac-
tors, evident both within a given batch
and between batches and seasons. By
contrast, the L . C.-type mix required no
prior preparation, and the mix could be
prepared for planting immediately upon
delivery of materials. Storage space for
compost piles was thus saved. Fertilizer
top dressing of the seedlings growing in
compost cost SO. 90 to SI. 10 per 1.550
flats, whereas application of calcium
nitrate i1^ oz. per gal. on a 10-day
schedule) to the L. C. mix cost only
SO. 35. an additional saving.
It was found in four tests that the
plants grown in the L. C. mix were
salable 5. 6. 9. and 11 days sooner than
by the old method. Time saved in this
way may mean that an extra crop can
be grown during the busy season. In
these instances the differences probably
were due both to damping-off and exces-
sive salts in the compost. Conductance
1 Sec. 4 1 of compost initially, and after 2
[265]
weeks, for the above series was: 6.4,
dropping to 3.7; 10.9, dropping to 5.4;
8.3, dropping to 5.8; 12.1, dropping to
6.9. The conductance of the U. C.-type
mix ranged from 2.2 to 2.6 initially and
1.7 to 1.9 after 2 weeks.
In the compost the root systems were
poorly developed and top growth was
very irregular (height varying by 1 to
1% in. in a single flat) , whereas plants
in the U. C.-type mix were uniform in
size (maximum variation % in.) and
color, and were larger.
Production in the compost was com-
plicated, requiring an experienced per-
son to water the flats, shifting from
heavy leaching to light applications as
the problem changed from salinity to
damping-off (fig. 35). Plant growth was
undoubtedly depressed, in turn, by this
practice, since celery is a "wet crop".
With the U. C.-type mix, a regular irriga-
tion schedule was set up that maintained
proper soil moisture, since neither
salinity nor damping-off was a problem.
The seedlings were transplanted to com-
mercial fields, where it was consistently
found that those grown in the mix re-
mained green and started growth more
quickly than those grown in the compost.
Despite the demonstrated effectiveness
of the system in this nursery, the nursery
management considered that it was
easier to continue in the old method and
too much trouble to change! His com-
petitors, however, did make the change.
POT AND FOLIAGE PLANTS
There is a large business in raising
pot plants both for retail sale in Califor-
nia and for shipping out of state. Foliage
plants have perhaps the fastest expand-
ing market of any florist crop today, and
the demand is largely filled from Cali-
fornia and Florida. Pot plants are grown
throughout the state, but there tends to
be a concentration of foliage crops in
southern and central California.
Nursery E . . .
is an important producer of pot and
foliage plants in central California. The
owners formerly used multiple soil
mixes, sometimes changing the type for
each crop, or for a given crop each year,
in search of something better. In 1953
they changed over to the U. C. system
of soil mixes and treatment. This has
been so successfully applied that mech-
anization has been adopted extensively;
the details of some of these methods are
presented in Section 1 7. Because of the
labor saving effected, four men are able
to do the work that formerly required
twelve to fourteen.
Two years of commercial experience
has demonstrated that practically all
types of foliage and blooming pot plants
grow very well under the U. C. system.
The cost of soil preparation has been
greatly reduced, and certainty of results
tremendously increased. The results have
been at least as good as before, and in
most cases superior.
The changeover introduced some
problems, however. Poinsettias planted
at the regular time grew so rapidly that
they were far too large for the average
market. The following season this was
easily corrected by delayed planting and
double pinching, a saving in time and
space then being realized. This nursery
is a successful advocate of the U. C.
system.
Nursery F
This southern California foliage-plant
grower began operations in 1948. It was
soon found that disease losses from soil
organisms constituted the principal
production problem. The losses from
[266]
Rhizoctonia were often complete, even
though the foliage was kept dry.
He tried to obtain clean stock from
various sources without success, and
was finally forced to produce it himself.
The success attained with Fittonia ver-
schaffeltii var. argyroneura under the
U. C. system illustrates the effectiveness
of the methods employed.
The planting stock was treated in hot
water by the methods explained in Sec-
tion 13, and then grown in individual
pots of steamed soil similar to a U. C-
type mix. The plants were grown to a
height of 6 inches under conditions of
general sanitation and without ever wet-
ting the foliage before cuttings were
taken. The cuttings were dipped in
Parzate and rooted in steamed sand. By
the time this procedure had been fol-
lowed for three generations, adequate
clean mother blocks had been estab-
lished. They have since been carefully
maintained and have yielded consistentlv
healthy stock.
At first the cuttings were rooted in
sand and planted in small pots, taking
8 to 10 weeks. Now the cuttings are
planted directly in small pots of U. C.
mix C (50 per cent peat). Automatic
misting of cuttings is practiced without
loss from diseases caused by Rhizoctonia
or water molds. Production of the fin-
ished plant ready for sale now requires
only 5 weeks. Over a quarter million
young plants are now raised annually
in scheduled production by this method.
Similar success has been obtained
with Peperomia obtusifolia var. varie-
gata, Peperomia sandersii, Pellionia pul-
chra, Nephthytis sp., Diefjenbachia picta,
D. bausei, and Hedera sp. (Glacier ivy)
by following the recommended proce-
dures for eliminating the diseases.
Nursery G . . .
is a small producer of foliage plants,
particularly Philodendron and Dieffen-
bachia, in central California. For many
vears clav soils mixed with leaf mold
J J
and manure were used. Growth was ir-
regular and consistent losses were ex-
perienced because of overfertilization
and poor drainage. Fortunately this
nursery is located on a Colma fine sand
deposit. The grower switched all of his
foliage plant operation to a I. C.-type
mix in 1953. and the above problems
were solved.
CAN-GROWN WOODY PLANTS
A large volume of nursery stock is
grown in cans (ranging from 1 to 5
gallons' capacity) in California, under
lath or glasshouses, or outdoors. This
stock is sold largely for home planting.
Nursery H . . .
a well-established wholesale nurserv in
central California, had been using soils
of various types, mainly clay. They
changed to a U. C.-type soil mix and
used methyl bromide fumigation, obtain-
ing 25 to 50 per cent increased growth
over their standard procedure in the first
season. The soil did not shrink away
from the can when irrigation was de-
layed as did the clav. making for easier
and more effective watering.
After part of a season of successful
growing, it was decided to try using rice
hulls, an inexpensive and abundant or-
ganic material in the area. The mix was
altered by omitting potassium, which
rice hulls supplied. The growth has been
excellent, containers are lighter in
weight, and cost of the mix has been
reduced.
[267]
BENCH AND BED CROPS
The flower crops grown in raised
benches and ground beds have enormous
value in California, among the more im-
portant being roses, carnations, chrysan-
themums, and gardenias. Because these
plants are large and deep-rooted and do
well in garden soils, it would be expected
that the benefits from using a U. C.-type
mix would be less than with the foregoing
crops.
Nursery I . . .
grows gardenias in raised benches in
southern California. Using a soil mix
composed largely of clay and peat, they
were having trouble with chlorosis and
death of plants. The soil steaming was
only partially effective, and salinity from
overfertilization and a poor water sup-
ply created an additional problem. They
tried a planting in U. C. mix C (50 per
cent peat) . Uniform, effective steaming
was obtained, with little or no evidence
of disease in the .2% years of the test.
The plants have grown very well, with
greatly increased production. The use of
an iron chelate in the winter (2 oz. per
100 sq. ft.) completely controls normal
cool-weather chlorosis. All of this firm's
plantings are now in this mix. The rather
poor-quality water is no longer a hazard.
In fact, they have expanded into the field
of foliage-plant growing, and now use
the same mix for stock beds and potted
plants.
Nursery J . . .
is a carnation grower in central Califor-
nia. On the basis of comparative trials of
a U. C.-type mix in raised beds as
against his standard clay loam, he has
shifted to the light mix for his entire
culture. Several outstanding benefits
have been observed at this nursery. Car-
nations in the U. C. mix showed a very
low percentage of calyx "splitting" as
compared to those grown in clay loam.
In addition, the frequency of irrigation
for the clay loam beds was almost twice
that for the U. C. mix. Further, the clay
loam upon drying developed deep cracks
which caused severe root shearing; this
was not evident with the U. C.-type mix.
Nursery K . . .
is a rose grower in central California.
The U. C.-type soil mix was tested in
several raised beds in a glasshouse. The
production was as good as in his usual
soil, a clay loam that had been in the
benches for twenty years. Because of re-
peated steaming and additions of peat
during this period the soil had been
brought into a good physical structure.
If the soil should have to be changed in
the benches for some reason, the nursery
plans to use a U. C.-type mix. The initial
physical structure of a U. C.-type mix
equals that attained by clay soil after
several years' improvement through
organic additions.
CYMBIDIUMS IN BEDS
Since World War II the growth of Nursery L .. .
cymbidiurns under glass or lath has be- raises cymbidiums in ground beds in
come important, particularly in southern southern California. The original soil
California. mix was completely organic, consisting
[268]
of leaf mold, manures, and bean straw.
The soil mix was placed in beds 12
inches deep on top of an adobe soil.
Within 2 years or less the beds shrank to
a depth of approximately 6 inches, owing
to decomposition of the organic mate-
rials. The nutritional level varied widely
throughout the nursery; some beds were
overfertilized, others were underferti-
lized. Because the nutritional levels were
unpredictable, it was impossible to set up
fertilizer applications on a regular sched-
ule. The over-all result was irregular
plant growth and production.
To correct this problem the nursery-
man changed to a soil mix consisting of
fine sand, peat moss, and pine shavings,
CAUTION:
Many
of
the i
:hemicals
mentioned
in this
manual
are
poi-
sonous and
may
be
harmful.
The
user should
carefu
lly
Follow the
pre-
cautions on
the 1
abe
Is of
the
con-
tainers.
with known nutrient leveis. The applica-
tion of fertilizer has been standardized
and placed on a simple, regular schedule.
The volume of the soil in the beds has
remained relatively constant. The over-
all results are reflected in uniform plant
growth and production and a simplifica-
tion of management practices. Cost of
preparing beds has been reduced.
LANDSCAPE APPLICATION OF THE U. C. SYSTEM
A large race track in southern Califor-
nia had a history of high weeding costs
and expensive replacement of plants
killed by disease. To overcome this
yearly loss the infield area of approxi-
mately 10 acres was treated with methyl
bromide (fig. 125) and subsequently
planted with disease-free stock pro-
duced under the U. C. system. Prior to
the field fumigation, even though dis-
ease-free stock was used, as many as
1,500 new plants were needed each week
Fig. 125. Left, methyl bromide fumigation of field soil in southern California for elimination
of pathogens and weeds. This is a field adaptation of the technique developed for glasshouse
soil treatment. Right, the same field 2 months after planting with seedling pansies which had
been grown in treated nursery soil. This illustrates the advantage of using healthy plants in clean
soil; a more vigorous planting results, and the soil is not reinfested by the planting stock.
to replace those killed by damping-off
fungi. After fumigation, only 400 plants
were replaced in a 4-month season, and
most of these were mechanically or
chemically injured. This illustrates the
necessity of both soil treatment and
clean plants in disease control (fig.
125). As another benefit from soil treat-
ment, weed control was reduced from
$60 per acre to a minor figure.
A landscape use of the U. C. system
was the replacing of heavy disease-
infested soil in confined beds with a
fumigated U. C.-type mix. The disease
control achieved was similar to that de-
scribed for the infield planting. Plants
grown in a treated sand-peat mix were
two to four times as large as the same
stock grown in the treated natural loam
of the infield. The use of a U. C.-type
soil mix in places where large beds are
to be filled with hauled soil seems to be
worthy of wider trial in public or private
plantings.
GENERAL EXPERIENCE
The results of grower experience with
the several aspects of the U. C. system
have shown that:
1. It is uniquely adapted to mecha-
nization.
2. It provides a continuous supply of
a uniform growing medium.
3. It permits the use of fewer and less
experienced laborers. These, how-
ever, should understand the "why"
as well as the "how" of what they
do, and should be directed by well-
trained supervisors.
4. It provides a means of avoiding
salinity difficulties.
5. The soil provides good aeration and
water drainage for root develop-
ment.
6. The disease problems are essentially
eliminated by the treatment of soil
and containers, the use of healthy
planting stock, and careful culture
to maintain them in that condition.
7. The cost of weeding is eliminated.
8. Post-steaming toxicity of soil is
avoided.
9. Tedious composting procedures are
eliminated.
10. A single basic mix replaces the
many formerly used.
11. Materials are employed that are
easily and cheaply obtained.
12. It enables the production of plants
that are more uniform, healthier,
and larger, at lower cost, more re-
liably, and faster than before.
[270]
SECTION
m
Mechanization
and the U.C System
J. W. Huffman
R. H. Sciaroni
Mechanizing an old nursery
Planning for mechanization
Stages in the flow of materials
Watering and fertilizing in the glasshouse
General comments
0
ne OF the major advantages of the tion with the Agricultural Extension
U. C. system for the nursery is the ease
with which this type of production may
be mechanized. Increased labor cost,
higher taxes, and real-estate subdivision
have made nurserymen anxious to attain
greater efficiency (Sec. 2). Residential
development has forced the discontinu-
ance of composting manure piles, be-
cause of their odor and fly problems.
The Agricultural Extension Service
realized that changes would have to be
made if urban nurserymen were to con-
tinue in business. The greatest potential
contribution seemed to lie in standard-
ization of soil mixes and mechanization
through the U. C. system.
During the developmental period of
the U. C. system, perhaps partly because
of it, intensive mechanization was begun
in a few California nurseries. In coopera-
Service and Experiment Station, they
adapted ideas from materials-handling
equipment in canneries, assembly lines,
sand and gravel operations, concrete-
mixing plants, and other well-engineered
installations. These pioneering growers
exhibited ingenuity and imagination in
devising equipment for their needs in
existing nurseries.
The methods and equipment de-
veloped have greatly reduced labor re-
quirements and enabled the substitution
of semiskilled for scarce highly skilled
labor in many jobs. Nursery mechaniza-
tion is still developing, and further im-
provements will certainly be made.
Since, however, there is such a pressing
need for greater efficiency in the nursery
industry, it is desirable that the tech-
niques thus far developed be presented
here.
[271]
SOIL TREATED IN CONTAINERS
Constituents of soil mixture clumped in piles or bins on delivery
I
Skip loader
I
Soil blended and moisture added in concrete mixer
I
Dumped direct or conveyer belt
ci . " c\\ , Untreated flats or pots
Flat or can filler ' — - — — —
Manual
Stacked on pallets
I
Forklift tractor
Steam treatments:
Piles of flats or cans covered
with tarpaulin (5).
Horizontal chamber with hood (10).
Horizontal steam vault (6).
Autoclave (9).
Chemical treatments:
Piles of flats or cans
covered with plastic sheet
and treated with methyl
bromide orchloropicrin
aerosol.
Forklift tractor
Piles unstacked by hand
I
Conveyer belts or rollers
Planted or seeded by hand
Machine planted or seeded
Conveyer belts or rollers
I
Growing area
Fig. 126 (both pages). Diagrams of vaiious methods for mechanization of thirteen ways to
treat soil with steam or chemicals in commercial California nursery practice. Numbers refer to
equipment types (Sec. 10). (From a chart by K. F. Baker.)
[272]
SOIL TREATED IN BULK
Constituents of soil mixture dumped in piles or bins on delivery
I
Skip loader
4<
Soil blended and moisture added in concrete mixer
Dumped direct or conveyer belt
V
/
Mobile
Mobile
bin
steam
types
i \
box (4)
Pulled
oy tractor
\
\
Bin
(2)
Dumped
durr
iped
direct
Mobile units
pulled by tractor
Stationary steam
box (4); may be
in tandem
Treated with chloro-
picrin in movable
or stationary bins
or boxes, or with
methyl bromide in
piles covered with
plastic sheet.
Dumped direct
or conveyer belt
I
Flat or can filler
Manual
Bin and
potting bench (3)
* Stacked on pallets
Forklift I tractor
Piles unstacked by hand
f—
Conveyer belts or rollers
\r
Horizontal revolving drum with
steam injected (28) or with
blow torch (30, 31).
Screw type with injected steam (29).
Flats or
pots treated
with steam or
chemicals.
Dumped into flats or cans, or
into flat or can filler.
Manual
Planted or seeded by hand
Machine planted or seeded
Conveyer belts or rollers
Growing area
[273]
MECHANIZING AN OLD NURSERY
While the greatest benefit from mech-
anization obviously is gained in a nur-
sery designed for it, impressive savings
have often been made by adoption in
existing nurseries of many of the proce-
dures outlined here. No matter how
small or poorly designed a nursery may
be, some of the mechanized methods de-
scribed will prove adaptable and profit-
able.
The grower should study the flow
diagrams of mechanization in nurseries
(fig. 126), the summary chart of types
of soil steamers (table 15), and the text
and illustrations in this section concern-
ing mechanization in California nur-
series. He should observe the practices
in several well-mechanized nurseries; his
farm advisor or the authors can, if de-
sired, suggest some to visit. From these
several sources profitable ideas adapt-
able to the specific nursery will be ob-
tained.
It will be found, furthermore, that
many of these methods may be adopted
independently and consecutively, with-
out major upheaval or expense (see
"Aids in Adopting the U. C. System,"
p. 1). Many nurserymen have demon-
strated that the U. C. system can be
adopted in progressive easy stages. It is
important, however, that the process be
continued until a complete program is
established, rather than stopping at
some intermediate level of partial
benefits.
PLANNING FOR MECHANIZATION
The exact manner of mechanization
must be developed for each nursery,
preferably before it is built. Because of
smog, population pressures, and tax
rates, many California nurseries may be
forced to move in the next several years,
house equipment) might well be em-
ployed. Some of the basic mechanization
methods presently used in a few nur-
series are outlined here and presented
in chart form (fig. 126).
Some of the factors which should be
and this affords an excellent opportunity considered in planning a new nursery
to properly design the new units for
efficient management. For this reason, it
is suggested that the central ideas of the
II. C. system be tested now, and that
thought be given to incorporating these
principles into any new construction.
Some of the books on mechanization
of materials handling (see Appendix,
References) should be consulted in the
initial stages of planning to be sure that
the besl modern methods are considered.
If (he unit is to be a large one, the
services of an engineer who specializes
in materials handling or in the design of
continuous processes I for example.
assembly lines, cannery and packing-
may be suggested. Careful attention
should be given to the soil-treatment
method and facilities to be used (sees.
8 through 11).
Utilizing a natural slope
If the land has a natural slope this
may be utilized by placing the soil piles
at the top, followed progressively down-
hill by the mixing equipment, container-
filling equipment, treatment facilities,
planting operations, and the growing
facilities. Gravity can then be made to
do much of the transportation work, by
using steel rollers.
[ 274 ]
Glasshouse arrangement
and design
Glasshouses should be arranged so
that they branch off both sides of a
central corridor through which tem-
porary steel rollers may be set up, lead-
ing from the soil area. Plans should in-
clude openings for steel rollers to run
into each house through the end wall,
rather than the doors. Containers may
then be taken almost directly to their
places in the glasshouse without exces-
sive lifting or carrying.
The width of the glasshouse aisles
should be considered in terms of the
equipment to be pushed through them,
and vice versa. One nursery decreased
the labor of emptying glasshouses by
designing them so that the sides were
removable down to bench level, to per-
mit the removal of flats through the sides
of the houses. Flats were moved on steel
rollers and loaded directly onto truck
beds (at the same height) for transporta-
tion to the area where the plants were
hardened-off before sale.
The size and orientation of the
benches should be studied for greatest
mechanization potential. If bench crops
are to be grown, the width of the benches
and any steam pans to be used should be
the same. Structural pipes through beds
should be avoided whenever possible, as
they invariably increase cost of steam
treatment.
Paving of yard
The area around all houses should be
paved to expedite mechanization and
reduce weed growth, from which insects,
often virus-carrying, move into the
glasshouses.
STAGES IN THE FLOW OF MATERIALS
Processing and Stockpiling
the Materials
Possible sources of the fine sand were
discussed in Section 6. A statewide sur-
vey for exact sources has been con-
ducted,1 and information on this may be
obtained through your local farm ad-
visor. It should be emphasized that the
various truckloads of the fine sand
should be checked on delivery for uni-
formity in conforming to physical (Sec.
6) and salinity (Sec. 4) standards, if
there is any reason to suspect variability.
To facilitate this, it is well to order this
material somewhat in advance rather
than wait until it is actually needed. Be-
cause of the storage space required, it is
not usual to stockpile large quantities.
Since no composting is necessary in pre-
^y M. H. Kimball, Ornamental Horticul-
turist, California Agricultural Extension Serv-
ice.
paring the mix, no space is required for
this process. Usually a supply sufficient
for 2 to 3 weeks is kept on hand. The
Canadian or German peat moss may be
obtained from your local horticultural
supply house.
Both of these ingredients should be
stored in bins under a roof, preferably
on a large concrete slab, or at least in a
well-drained area. This structure might
well be large enough also to accommo-
date the mixing operation. There would
then be only short hauls between the dif-
ferent steps of this procedure, and opera-
CAUTION:
Many
of the <
:hemicals
mentioned
in this
manual
are
poi-
sonous and
may
be harmful.
The
user should
carefu
Ily follow the
pre-
cautions on
the 1
abels of
the
con-
tainers.
[275]
tions could continue during rains. This
building should be separated from the
soil-sterilizing and planting facilities in
order to reduce recontamination, and
should be located for greatest conveni-
ence in carrying the soil or the filled
containers to the soil-treatment equip-
ment and glasshouses.
Storage of Soil
The U. C. mixes may be stored in-
definitely if organic nitrogen has not
been added, but should not be held more
than a week if they contain more than a
small amount of such material (sees. 5
and 7). Soil is preferably stored before,
rather than after treatment to reduce the
recontamination hazard. Some growers,
however, have satisfactorily stored
treated soil in a tight building where
wind-blown soil will not reach it (fig.
128). Such a structure should not be
near the mixing operations. The build-
ing should be humidified, perhaps by
mist nozzles, to reduce drying of the soil
if prolonged storage is contemplated.
Raising humidity to prevent drying of
flats is preferred to direct watering,
which is extremely difficult since the
flats are stacked on pallets. Watering be-
fore use also has a tendency to compact
the flats and cause the transplanter to go
through an unnecessary step of loosen-
ing the soil before transplanting.
Excellent temporary storage is pro-
vided by placing a tarpaulin over the
stacked flats. The flats should be kept out
of the sun.
Making Flats
In one large nursery, a sufficient num-
ber of flats was used so that it was
economic to purchase a box-making
machine especially designed for south-
ern California flats. This reduced hand-
construction and hence costs. Several
smaller nurseries might go together in
purchasing such equipment, or a port-
able unit might be taken, on a service
basis, from one nursery to another to
prepare the season's supply.
Preparing the Soil Mix
Equipment needed
The presently accepted and generally
adopted method for preparing nursery
soils is to use a stationary concrete
mixer for about a 10-minute period.
These are available, new or used, in
various sizes. The larger sizes have a
loading apron into which the ingredients
are conveniently dumped by a skip-
load tractor. Used transit-type mixers
(figs. 127 through 130) with a capacity
of about 5 cubic yards are commonly
utilized. They cost $400 to $800 and must
be cleaned of cement, reconditioned, and
painted before use. Small nurseries use
1- to 2-cubic-yard cement mixers. Several
growers use two mixers to reduce the
time of the operation.
Some nurseries have tried mixing
their soil with a skip loader and screens,
but have found this unsatisfactory.
An important benefit of the U. C.
system is that no complicated equipment
is required for breaking up clods. //
hard lumps of soil are present in the fine
sand, it is not of the proper type (Sec.
6). Several nurseries in central Califor-
nia have each recently spent $800 to
$1,000 for equipment to break up the
lumps in the clay soil before mixing
could begin.
The only equipment used for prepar-
ing the ingredients for a U. C.-type mix
is a small shredder sometimes employed
for breaking up the bales of peat. More
frequently the peat is wetted and is
broken up by a fork.
If the soil contains debris or rocks it
may be screened at this time (rare), or
after mixing (see below).
Mixing
The fine sand and moistened shredded
peat, as well as the proper weights of
the desired amendments and fertilizers
(sees. 5, 6, and 7) are dumped into the
mixer in their proper relative propor-
tions. During the rotations of the mixer
[276]
,
.##&&
Fig. 127. General view of a bedding-plant nursery, showing the mechanization of soil handling.
Transit mixers (A) mix the soil ingredients, which are then conveyed (B) to a rotating screen (C)
above the flat filler (D). The flats are carried on steel rollers (E) under the filler, and are stacked
on pallets (F), which are transported by the fork-lift (G) to the steam chamber.
Fig. 128. Another view of the same soil-handling operation. The steam chamber (H) is shown
in use. If soil is to be stored temporarily, it is moved to the enclosed building (I) by the fork-lift.
The peat supply and empty flats are shown in the foreground, the fine sand is to the immediate
left (not shown).
a measured amount of water is some-
times added to bring the mix to a uni-
form desired moisture content for steam-
ing and planting (Sec. 8) . It is generally
preferable, however, to moisten the in-
gredients before mixing. A ribbon mixer
of the type used in mixing plaster has
proved excellent for soil.
If adequate storage space is planned,
the nursery may use the soil-mixing and
container-filling equipment only 2 to 3
days a week, using two or three men.
Note, however, that the mix containing
organic nitrogen should not be stored
for longer than a week before planting
(sees. 5 and 7) .
It requires about 30 minutes to han-
dle a load in concrete mixers. Thus the
capacity in cubic yards, multiplied by 2,
will give the hourly capacity.
If the mix is not to be screened, it may
be taken from the mixer directly or car-
ried by a conveyor belt or skip-load
tractor (see "Transporting the Soil," be-
low) directly to the flat filler, to the
treatment equipment (if it is to be
treated in bulk), or to a combined bin
and potting bench (Sec. 10).
Screening
When the soil is mixed it is sometimes
dumped directly onto a moving belt that
conveys it to a revolving circular screen
8 to 10 feet high (figs. 127, 128, and
130). These units are custom-made for
each nursery and cost about $1,500. The
belt width is about 16 inches, and the
unit is driven by a gasoline engine or
electric motor. The screen is 3 to 4 feet
in diameter and 5 to 6 feet long. Usually
there is little debris in the ingredients
and this procedure is done as much to
continue mixing as to get rid of stones,
sticks, rubbish, or large pieces of peat.
The mix may fall through the screen di-
rectly into the hopper of the flat filler, or
into a pile.
Fig. 129. Method of filling a transit mixer by means of a skip loader. The proportion of fine
sand and moistened peat is determined by the number of loads of each. The tandem arrange-
ment of mixers assures a continuous output of mixed soil.
Filling the Containers
It is generally desirable to place the
soil in the containers prior to treatment.
Sometimes, however, the sequence may
at this point be reversed. The soil is then
treated in bulk before it is placed in con-
tainers that have been treated separately.
Treated soil should never be placed in
untreated containers.
The flat filler (fig. 130) or container
fillers (figs. 10 and 135) vary more in
construction than other pieces of equip-
ment used in the mechanized nursery. In
general they consist of a wide-mouth
tapered hopper, the soil flowing through
the adjustable opening onto a variable-
speed rubber belt. The soil drops from
the end of this belt into a flat or other
container below, that is carried on an-
other belt moved by power or manually.
The width of the lower opening of the
hopper and the width of the belts may be
varied for different types of containers.
Flat fillers
Some of the flat fillers use an auger
gear or leveling bar to level the soil in
the flats. Some of these devices will han-
dle 900 flats per hour. One man is re-
quired to place the flats on the input
conveyor belt, and one to remove the
filled flats at the output. Flats are usually
stacked on hardwood pallets (figs. 127
and 130) (36 by 54 in.) to be transported
by a fork-lift tractor (fig. 127). The
price of this type of equipment is about
$1,000; the hardwood pallets are about
$2.75 apiece.
This step may be difficult to mechanize
if flats are not of uniform size or have
wide bottom cracks. Paper liners are
sometimes used in such old flats. In
southern California the flats are uni-
formly 18 by 18 by 3 inches; those in
central California are quite variable in
size. This latter situation is, of course,
an obstruction that must be resolved if
Fig. 130. Detail of screening and filling operation, showing transit mixer (A), conveyor belt
(B), rotating screen (C), flat filler (D), and steel rollers (E). The worker is removing flats from the
steel rollers and placing them on a pallet. Note the wood separator strips (arrow), which are
placed between layers of flats.
economical mechanization is to be
adopted.
Mechanical can and pot fillers
Mechanical fillers are available (see
Appendix) for 1-gallon cans and pots
(fig. 135) and for 2- and 5-gallon cans
(fig. 10). Soil may be conveyed to this
equipment after being mixed, and
screened and treated in bulk; the filled
containers are planted at once.
Hand-filling
Some nurseries fill the containers by
hand at the point of mixing. They may
then be piled on pallets as before and
carried by a fork-lift tractor. However
filling may be done, the number of flats
placed on the pallet will depend on the
size of the tractor, the size and shape of
the containers, and the dimensions of
the treatment chamber.
Mobile bin and potting bench
In one nursery, the soil from the
mixer is dumped onto a mobile bin and
potting table (Sec. 10, type 3) . This flat-
bed wagon (fig. 132) has a movable
tongue hitch, and can easily be pulled
by a light truck or tractor. Perforated
pipe is permanently mounted in the bot-
tom of the wagon and is easily con-
nected to the generating source for
steaming. It is covered by a tarpaulin
during this process. After steaming it is
pulled into the potting headhouse. In a
few hours the soil is cool, and one side
of the wagon is let down for a work
table. Potting and planting are done di-
rectly from the treated pile. The soil mix
is easily worked into pots around bulbs
or rooted plants.
Treating Soil and Containers
The details have already been given
for steam treatment (sees. 8, 9, and 10)
and chemical treatment (Sec. 11) of
nursery soils. Equipment has been de-
scribed (Sec. 10) for steaming of the
-oil. Chemical treatment is generally
done in stacks of staggered flats or on
wooden pallets. In either case, treatment
operations are preferably isolated from
those of soil mixing or flat filling to re-
duce possible recontamination.
The cost of materials and labor for
constructing a steam chamber (figs. 128
and 131 ) varies from $250 to $500, ac-
cording to the type and size of installa-
tion. Marine plywood (waterproof glue)
sheets % inch thick and 4 by 10 feet in
size should be used for sides, doors, and
top. Exterior plywood is not suitable for
this purpose. The frame is constructed
of either metal or 2 by 4 lumber. De-
tails on this and other types of equipment
are given in Section 10.
Transporting the Soil
Untreated soil
Untreated ingredients are most eco-
nomically transported by a skip-load
tractor (figs. 126 and 129) from storage
piles into the soil mixer. From there the
mix may again be transported by a skip-
loader or be carried by a moving rubber
conveyor belt to the flat filler, or car-
ried by a rubber belt to the revolving
screen, from which it is dumped into the
flat filler. Alternatively, the mixed soil
may be taken by skip-loader to a bulk
steam treater, or the steamer (if mobile)
may be brought under the mixer and
screen and filled.
Filled containers
Containers are usually stacked on
wooden pallets and carried by a fork-
lift tractor (figs. 127 and 131). The cost
of this piece of equipment is variable,
depending on the size of the unit; a
large unit with pneumatic tires used by
some nurseries costs $3,200 to $3,500.
Since the fork-lift is efficiently used
in many nursery operations, its cost
should not be completely charged to
soil handling. At one large pot-plant
nursery the fork-lift mounted at the rear
[280]
Fig. 131. Loading a pallet of filled flats into a
wooden vault (type 6, Sec. 10) steam chamber
by means of a fork-lift. The vault is unloaded
in the same manner, and taken by fork-lift to
the seeding or planting operation.
Fig. 132. Mobile bin and potting bench (type
3, Sec. 10), showing the potting operation. The
soil is dumped into the bin from an elevated
transit mixer and steamed from pipes in the
bottom of the wagon, which is then pulled to
the potting area. With this type of equipment
care must be exercised to avoid introducing
pathogens into the exposed soil mass from oc-
casional diseased propagating material during
the potting operation.
Fig. 133. Bicycle-wheel cart used for trans-
porting potted stock into the glasshouse from
the potting bench. This is adaptable to glass-
houses with narrow aisles or where conveyor
belts are not practical.
Fig. 134. Rack for transporting pots to a
vault-type steamer, or to be covered with a
tarp and steamed or treated with methyl bro-
mide. Unit is transported by a fork-lift tractor.
of the tractor is used to transport steri-
lized clay pots (fig. 134).
The containers may be taken from the
treatment chamber by the fork-lift trac-
tor on the same pallets, to the place
where they will be planted. They may,
however, be carried either on steel rollers
or a conveyor belt. After planting they
generally are taken on portable steel
rollers to their location in the glass-
house, sections of rollers being removed
as the house is filled.
A special cart equipped with bicycle
wheels (fig. 133) has been constructed
for use with the mobile bin and potting
bench mentioned above. The cart has a
low center of gravity for good balance,
and the narrow bed facilitates rapid
transit of planted pots through glass-
house aisles.
Planting
Transplanting seedlings
Planting is an extremely varied opera-
tion. It varies from transplanting of
seedlings into flats by hand, an opera-
tion that seems to defy mechanization,
to planting them in pots. The latter op-
eration has been mechanized by the
Erdprinz planter in Germany (see Ap-
Fig. 135. Automatic can or pot fillers for placing soil in 1-gal. containers and forming a cen-
tral depression into which the liner is planted. (See also fig. 10.) (Photo courtesy of Oki Nursery,
Perkins, California.)
[ 282 1
pendix) and equipment for use with the
U. C. mixes has been developed in Cali-
fornia (figs. 10 and 135).
Machine-seeding
Equipment has been used from time
to time for spot-planting the seed in con-
tainers. One unit was used for several
years for such planting of pepper seeds
in flats. It consisted of a vacuum plate
that fitted the inside dimensions of the
flat, and had a hole drilled where each
seed was desired. This plate was alter-
nated between a tray of clean seed (with
the vacuum on) and a flat (with the
vacuum then released). It was possible
to seed 150 flats per hour in this way.
The seed and soil were covered with tis-
sue paper, then by sterile clean sand, and
watered generously. Similar planting
plates are available on special order
(see Appendix).
Mechanical seeders of this type will
not operate efficiently on tiny seed, and
attempts to evade this by pelleting the
seed to larger size plunge one into germi-
nation difficulties. In one series of tests
by P. A. Chandler (unpublished data),
pelleted seeds of Theodosia Improved
petunia gave best germination when they
were placed on the surface, pressed
lightly into the soil, and then sprinkled.
All other methods were quite inferior.
The germination difficulties and dif-
ferences in seed size, vitality, and germi-
nation time have all indicated a dubious
future for pelleting of fine seed.
An experimental mechanical seeder
recently seen may solve these difficulties.
Until one is perfected, fine-seeded plants
will require hand-transplanting. For
large-seeded plants machine-seeding has
for several years been an accomplished
fact.
WATERING AND FERTILIZING IN THE GLASSHOUSE
In some cases it has been satisfactory
to water flats in the glasshouse by over-
head sprinklers. Because of the excellent
drainage of a U. C.-type soil mix and
freedom from damping-off fungi, there
is little danger from applying excess
water. Thus, enough water can be ap-
plied to satisfactorily wet nearly all of
the flats, and the few that need more can
be hand-watered. This procedure saves
Fig. 136. Liquid-fertilizer injector for accurately diluting nutrients into the water stream during
irrigation. (Photo courtesy of Smith Precision Products Co., South Pasadena.)
[283]
much labor, but can only be used when
a whole glasshouse area is reasonably
uniform.
Some growers have applied fertilizer
through such a system. One grower of
Kentia palms successfully fertilized in
this way for several years. Another
grower of pot foliage plants has also ob-
tained excellent results, using a fertilizer
injector (fig. 136) in the water line.
Care must be taken to flush the chemical
from the pipes.
A better procedure is probably pro-
vided by hand application of liquid
fertilizer by means of special injectors
(fig. 136 and Appendix) which operate
through the watering hose. Fertilizers
may also be applied to the surface of
soil in pots in the dry form (sees. 5, 6,
and 7) .
GENERAL COMMENTS
The total cost of mechanizing the soil-
mixing process is about $6,000 to
$8,000, according to the size of the nurs-
ery. To avoid this large initial invest-
ment, most nurserymen with establish-
ments already built, develop one or two
steps at a time, beginning with the ce-
ment mixer. Each subsequent operation
is developed and designed for the spe-
cific operation. This partly explains the
wide variation in types of equipment
used in California.
Results from mechanization have gen-
erally been outstanding in producing
better plants at lower cost. It is often
found that two to three men working 2
or 3 days a week are taking care of all
soil mixing in a nursery that formerly
required six or more working all week
for this operation. Sometimes the saving
is even greater.
The nursery has yet to be built that
fully utilizes all the potentialities of the
U. C. system. Will yours do this?
[284]
N D I X
REFERENCES
Section 2
California State Commission of Housing
1954. California housing. California State Dept. Indus. Relations, Div. Housing, p. 13, 15.
Los Angeles County Chamber of Commerce, Agricultural Department
1955. Southern California agriculture ; 1954 — the year in review, p. 4.
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1953. Farm land disappears. 4 p. California Agr. Ext. Sen., San Mateo Co.
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1950. Statistical abstract of the United States 1930: 35.
1951. Statistical abstract of the United States 1951: 31.
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Section 3
Baker. K. F.
1946. Observations on some Botrytis diseases in California. Plant Dis. Reptr. 30: 145-55.
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Baker, K. F., and R. H. Sciaroni
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Beach, W. S.
1949. The effects of excess solutes, temperature and moisture upon damping-off. Pennsvlvania
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Chitwood. B. G.. and W. Birchfield
1956. Nematodes, their kinds and characteristics. Florida State Plant Board Bui. 2 (9) : 1—49.
Ellis. D. E.. and R. S. Cox
1951. The etiologv and control of lettuce damping-off. North Carolina Agr. Exp. Sta. Tech.
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Filipjev. I. N.. and J. H. S. Stekhoven, Jr.
1941. A manual of agricultural helminthology. 878 p. E. J. Brill, Leiden, Netherlands.
Goodey, T.
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Gravatt, G. F.
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McClure, T. T., and W. R. Robbins
1942. Resistance of cucumber seedlings to damping-off as related to age, season of year, and
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Section 4
Baker, K. F., O. A. Matkin, and L. H. Davis
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Hunter, J. A.
1952. Comparison of growth of tomato plants in impervious plastic pots and porous clay pots.
New Zealand Jour. Sci. Tech., Sec. A, 34: 365 68.
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1953. Increased profits through correct soil salinity. Pacific Coast Nurseryman 12 (9) :
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McCormick, J. A.
1949. Germination failure of shallow-seeded vegetable crops. California Agr. Ext. Serv., Mon-
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Pearson, H. E.
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242-48.
Richards, L. A., editor.
1954. Diagnosis and improvement of saline and alkali soils. U. S. Dept. Agr., Agr. Handbk.
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Schoonover, W. R., S. Wilhelm, and R. H. Sciaroni
1952. Testing greenhouse soils for soluble salts. California Agr. Ext. Serv. Pub. 6 p.
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1949. Soluble salt injury to gardenia. California Agr. 3 (12) : 5, 12.
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Aldrich, D. G., and J. P. Martin
1952. Effect of fumigation on some chemical properties of soils. Soil Sci. 73: 149-59.
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\ \om IIOUS
1948. Partial sterilization. Soils and Fort. 11 (6) : 357 60.
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\ 286 1
Bayer, L. D.
1956. Soil physics. 3d ed. 489 p. John Wiley and Sons, Inc., New York, N.Y.
Bonner, J., and A. W. Galston
1952. Principles of plant physiology. 499 p. See specifically p. 11-73. W. II. Freeman and Co.,
San Francisco, Calif.
Bouyoucos, G. J.
1936. Directions for making mechanical analyses of soils by the hydrometer method. Soil Sri.
42: 225-30.
California State Division of Mines
1956. Peat. California State Div. Mines, Mineral Inform. Serv. 9 (12) : 1-5.
Chandler, P. A.
1952. The U. C. soil mix for nurseries in California. Pacific Coast Nurseryman 11 (1) :
15, 40-42.
Clements, H. F., G. Shigeura, and E. K. Akamine
1952. Factors affecting the growth of sugar cane. Hawaii Agr. Exp. Sta. Tech. Bui. 18: 1-90
Danhardt, W., and H. Ramsch
1955. Keimgehalt der Torfkulturerden und der sogenannten Einheitserde. Deut. Gartenbau
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Davies, J. N., and 0. Owen
1951. Soil sterilization. I. Ammonia and nitrate production in some glasshouse soils following
steam sterilization. Jour. Sci. Food Agr. 1951: 268-79.
Feustel, I. C.
1939. The present status of research relating to the use of peat and muck as soil amendments.
Soil Sci. Soc. Amer. Proc. 4: 271-74.
Feustel, I. C, and H. G. Byers
1936. The comparative moisture-absorbing and moisture-retaining capacities of peat and soil
mixtures. U. S. Dept. Agr. Tech. Bui. 532: 1-26.
Fruhstorfer, A.
1952. Die Entwicklung der Einheitserde. Gartenwelt 52: 270-71.
Fujimoto, C. K., and G. D. Sherman
1948. Manganese availability as influenced by steam sterilization of soils. Amer. Soc. Agron.
Jour. 40: 527-34.
Haas, A. R. C, and J. N. Brusca
1954. Biuret, toxic form of nitrogen. California Agr. 8 (6) : 7, 11.
Hewitt, E. J.
1951. The role of the mineral elements in plant nutrition. Ann. Rev. Plant Physiol. 2: 25-52.
Hurerty, M. R.
1945. Compaction in cultivated soils. Amer. Geophys. Union Trans. 1944: 896-99.
Jones, L. H.
1931. Effect of the structure and moisture of plant containers on the temperature of their soil
contents. Jour. Agr. Res. 42: 375-78.
Jones, L. H., and H. D. Haskins
1935. Distribution of roots in porous and nonporous plant containers. Plant Physiol. 10:
511-19.
Kramer, P. J.
1949. Plant and soil water relationships. 347 p. McGraw-Hill Book Co., Inc., New York, N.Y.
Lawrence, W. J. C.
1956. Soil sterilization. 171 p. George Allen and Unwin Ltd., London, England.
Lawrence, W. J. C, and J. Newell
1950. Seed and potting composts with special reference to soil sterilization. 4th ed., 166 p.
George Allen and Unwin Ltd., London, England.
Longley, L. E.
1935. The value of peat in a potting soil mixture. Amer. Soc. Hort. Sci. Proc. 32: 639 1 \.
Lunt, H. A.
1955. The use of woodchips and other wood fragments as soil amendments. Connecticut Acr.
Exp. Sta. Bui. 593: 1-46.
Lunt, O. R., and B. Kwate
1956. Potassium frit as a special-purpose fertilizer. Soil Sci. 82: 3-8.
Lunt, 0. R., and S. J. Richards
1952. The oxygen and water relations of nursery soils. Pacific Coast Nurservman 11 (7):
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1932. The nature and properties of soils. 428 p. See specifically p. 389-96. Macmillan Co.,
New York, N.Y.
Maatsch, R.
1952. Einheitserde im Zierpflanzenbau. Siiddeut. Erwerbsgartner 6: 442.
McCool, M. M.
1932. Value of peats for mineral soil improvement. Boyce Thompson Inst. Contrib. 4: 245-55.
1936. Composts. Boyce Thompson Inst. Contrib. 8: 263 81.
1918. Studies on pll values of sawdusts and soil-sawdust mixtures. Boyce Thompson Inst.
Contrib. 15:279-82.
Millar, C. E., and L. M. Turk
1951. Fundamentals of soil science. 2d ed. 510 p. See specifically p. 234. John Wiley and Sons,
Inc., New York, N.Y.
Ml LDER, E. G.
1950. Mineral nutrition of plants. Ann. Rev. Plant Physiol. 1: 1-24.
Naville, E. II.
1913. The temple of Deir el Bahari, Part III. Egypt. Explor. Fund Mem. 16: 12-15, 17, pi.
LXIX, LXXIV, LXXIX.
Oberbacher, M. J.
1954. A chlorosis of citrus produced by biuret as an impurity in urea. Florida State Hort. Soc.
Proc. 67: 67-69.
OvERSTREET, R., and L. Jacobson
1952. Mechanisms of ion absorption by roots. Ann. Rev. Plant Physiol. 3: 189-206.
Rai, G. S., C. L. Hamner, and R. L. Cook
1956. Effect of biuret on bean plants grown in different soil types. Michigan Agr. Exp. Sta.
Quart. Bui. 39: 88-96.
Richards, L. A., editor.
1954. Diagnosis and improvement of saline and alkali soils. U. S. Dept. Agr., Agr. Handbk.
60: 1-9, 16-18, 31, 34-39, 65-82.
Uoiunson, R. R.
191-4. Inhibitory plant growth factors in partially sterilized soils. Amer. Soc. Agron. Jour.
36: 726-39.
Sanford, W. (;., 1). P. Gowing, H. Y. Young, and R. W. Leeper
1954. Toxicity to pineapple plants of biuret found in urea fertilizers from different sources.
Science 120: 349-50.
Shanks, J. B.
1955. Is manure dangerous? Maryland Florist (College Park, Md.) No. 23: 1-4.
SPRACUE, H. B., and J. F. Marrero
1931. The effect of various sources of organic matter on the properties of soils as determined
by physical measurements and plant growth. Soil Sci. 32: 35-50.
Starostka, R. W., and K. G. Clark
1955. Greenhouse evaluation and nitrification characteristics of biuret and urca-biuret mix-
tures. Agr. Chem. 10 (10) : 49-50, 103, 105.
\ i [HMEYER, F. J., and A. II. I Ikindrickson
L950. Soil moisture in relation to plant growth. Ann. Rev. Plant Physiol. 1: 285-304.
\V ilker, T. W., and R. Thompson
1919. Sonic observations on the chemical changes effected by the steam sterilization of glass-
house soils. Jour. Hort. Sci. 25: 19-35.
WlEBE, J.
1955. Phytotoxieity as a result of heat treatment of soil. 88 p. Thesis, Cornell University,
Ithaca, N.l . Abst. in: Dissertation Abs. 16: 7. 1956.
\\ im.ock, II. F.
I'm. Excavations ;it Deir el Bahri, 191 I L931. p. 49-51, 72, 84. Macmillan Co., New York, N.Y.
\\ OODH \ Ms- I). II.. and T. T. KOZLOWSKI
L954. Effects of soil moisture stress on carbohydrate development and growth in plants. Amer.
Jour. Hot. 11: 316 20.
| 2l\i\ |
Section 7
Bonner, J.
1950. Plant biochemistry. 537 p. See specifically p. 222-44. Academic Press Inc., New York,
N.Y.
Bonner, J., and A. W. Galston
1952. Principles of plant physiology. 499 p. See specifically p. 253-84. W. H. Freeman and
Co., San Francisco, Calif.
Bi rkhart, L.
1934. Metabolism of etiolated seedlings as affected by ammonium nutrition. Plant Physiol. 9:
351-58.
Clark, K. G.
1952. Urea-form — new nitrogen fertilizer. Crops and Soils 4 (8) : 14-15.
Davies, J. N.
1954. Steam sterilization studies. Cheshunt Exp. Res. Sta. Ann. Rept. 39: 47-53.
1956. Steam sterilization studies. Cheshunt Exp. Res. Sta. Ann. Rept. 40: 54-58.
Davies, J. N., and 0. Owen
1952. Steam sterilization studies. Cheshunt Exp. Res. Sta. Ann. Rept. 37: 67-78.
Duisberg, P. C, and T. F. Buehrer
1954. Effect of ammonia and its oxidation products on rate of nitrification and plant growth.
Soil Sci. 78: 37-49.
Grogan, R. G., and F. W. Zink
1956a. Fertilizer injury and its relationship to several previously described diseases of lettuce.
Phytopathology 46: 416-22.
19566. Fertilizer injury to lettuce. Damage reproduced by application of toxic concentrations
of inorganic commercial fertilizer materials or animal manure. California Agr. 10
(12) :5, 12, 16.
Hewitt, E. J.
1952. Sand and water culture methods used in the study of plant nutrition. Commonwealth
Bur. Hort. Plant. Crops Tech. Comm. 22: 1-241.
Klein, R.
1956. Nitrification in steam-sterilized soil. Cheshunt Exp. Res. Sta. Ann. Rept. 40: 29-32.
Lawrence, W. J. C, and J. Newell
1950. Seed and potting composts, with special reference to steam sterilization. 4th ed. 166 p.
George Allen and Unwin Ltd., London, England.
Long, M. I. E., and G. W. Winsor
1956. Urea-formaldehyde compounds as nitrogenous fertilizers. Cheshunt Exp. Res. Sta. Ann.
Rept. 40: 43-49.
Lorenz, O. A.
1956. Aqua and anhydrous ammonia, good sources of nitrogen fertilizers but materials should
be placed well away from plants to lessen chance of injury. California Agr. 10 (11) : 7.
Owen, O., and J. N. Davies
1950. Steam sterilization studies. Cheshunt Exp. Res. Sta. Ann. Rept. 35: 63.
Owen, O., and D. W. Rogers
1947. The availability of nitrogen in some organic fertilisers. Cheshunt Exp. Res. Sta. Ann.
Rept. 32: 66-70.
Owen, O., and G. W. Winsor
1948. Nitrification studies. Cheshunt Exp. Res. Sta. Ann. Rept. 33: 69-80.
1949. Nitrification studies. Cheshunt Exp. Res. Sta. Ann. Rept. 34: 62-70.
Owen, 0., G. W. Winsor, and M. I. E. Long
1952. The properties of some urea-formaldehyde materials in relation to their possible use as
nitrogenous fertilizers. Jour. Sci. Food Agr. 3: 531-41.
Thiegs, B. J.
1955. Effect of soil fumigation on nitrification. Down to Earth (Midland, Mich.) 11 (lj : 14—15.
Tiedjens, V. A., and W. R. Robbins
1931. The use of ammonia and nitrate nitrogen by certain crop plants. New Jersey Agr. Exp.
Sta. Bui. 526: 1-46.
[289]
Weissman, G. S.
1951. Nitrogen metabolism of wheat seedlings as influenced by the ammonium :nitrate ratio
and the hydrogen-ion concentration. Amer. Jour. Bot. 38: 162-74.
Wood, J. G.
1953. Nitrogen metabolism of higher plants. Ann. Rev. Plant Physiol. 4: 1-22.
Sections 8 and 9
Ball, V.
1953. Modern methods of steaming soils. Grower Talks (West Chicago, 111.) 17 (4) : 1-7;
(5) : 1-7.
1956. Soil sterilizing. Grower Talks (West Chicago, 111.) 20 (1): 1-11; (2): 16-22;
(3) : 15-20. Also in: Ball Red Book, ed. 9. p. 26-48. 1957.
Baver, L. D.
1956. Soil physics. 3d ed. 489 p. John Wiley and Sons, Inc., New York, N.Y.
Beachley, K. G.
1937. Combining heat and formaldehyde for soil treatment. Pennsylvania Agr. Exp. Sta.
Bui. 348: 1-19.
Bewley, W. F.
1939, 1948. Practical soil sterilization with special reference to glasshouse crops. Brit. Min. Agr.
Fisheries Bui. 22: 1-29 (3d ed.) ; 1-22 (4th ed.).
Bosworth, R. C. L.
1952. Heat transfer phenomena. The flow of heat in physical systems. 211 p. John Wiley and
Sons, Inc., New York, N.Y.
Bouyoucos, G. J.
1913. An investigation of soil temperature and some of the most important factors influencing
it. Michigan Agr. Exp. Sta. Tech. Bui. 17: 1-196.
1915. Effect of temperature on some of the most important physical processes in soils.
Michigan Agr. Exp. Sta. Tech. Bui. 22: 1-63.
Brown, C. A. C, and P. Wakeford
1947. Electrical soil sterilization by immersion heaters. Brit. Elect. Allied Indus. Res. Assoc.
Tech. Rept. Ref. W/T 14: 1-17.
BUEHRER, T. F.
1932. The movement of gases through the soil as a criterion of soil structure. Arizona Agr.
Exp. Sta. Tech. Bui. 39: 1-57.
Bunt, A. C.
1954, 1955. Steam pressure in soil sterilization. I. In bins. II. Glasshouse in situ sterilizing.
Jour. Hort. Sci. 29: 89-97; 30: 43-55.
1955. Steam-air mixture. John Innes Hort. Inst. Ann. Rept. 45: 28.
Bunt, A. C, and W. J. C. Lawrence
1955. Balanced steaming of glasshouse soil. John Innes Hort. Inst. Lflt. 14: 1-7.
Dimock, A. W., and K. Post
1944. An efficient labor-saving method of steaming soil. New York (Cornell) Agr. Ext. Bui.
635: 1-7.
Emerson, P.
1930. Principles of soil technology. 402 p. Macmillan Co., New York, N.Y.
Fishenden, M., and O. A. Saunders
1950. An introduction to heat transfer. 205 p. Oxford Univ. Press, London, England.
Frank, B.
1888. Ueber den Einfluss, welchcn das Sterilisiren des Erdbodens auf die Pflanzen-Entwicke-
lung ausiibt. Dent. Bot. Gesellsch. Ber. 6 ( General versammlungber.) : 87-97.
Hall, C. W.
1955. Which fuel for your boiler? Michigan Florist (Lansing, Mich.) No. 292 : 24.
Ho \kk, E. R.
1953. Temperature measurement with special reference to frost, steam sterilization and glass-
bouse climates. 13th Internatl. Hort. Cong. Kept. 2: 843 53.
Johnson, J \ mes
1916. Soil-steaming for disease control. Soil Sci. 61: 83 91.
[ 290 |
Keenan, J. H., and F. G. Keyes
1936. Thermodynamic properties of steam, including data for the liquid and solid phases.
89 p. John Wiley and Sons, Inc., New York, N.Y
Kersten, M. S.
1949. Thermal properties of soils. Univ. Minnesota Engineering Exp. Sta. Bui. 28: 1-227.
Lawrence, W. J. C.
1956. Soil sterilization. 171 p. George Allen and Unwin Ltd., London, England.
MacLean, J. D.
1930. Studies of heat conduction in wood. Results of steaming green round southern pine
timbers. Amer. Wood-Preserv. Assoc. Proc. 26: 197-217.
Morris, L. G.
1954a. The steam sterilising of soil. Experiments on fine soil. Brit. Nat'l Inst. Agr. Engin. Rept.
14: 1-32.
19546. The steam sterilising of soil. The application of research to practice. Brit. Nat'l Inst.
Agr. Engin. Rept. 24: 1-22.
Morris, L. G., and F. E. Neale
1957. The steam sterilising of soil: the heating of deep soil and the surface. Brit. Nat'l Inst.
Agr. Engin. Tech. Memo. 114. (In press.)
Morris, L. G., and K. W. Winspear
1957. The steam sterilising of lumps of soil. Brit Nat'l Inst. Agr. Engin. Tech. Memo. 113.
(In press.)
Newhall, A. G.
1930. Control of root-knot nematode in greenhouses. Ohio Agr. Exp. Sta. Bui. 451: 1-60.
1940. Experiments with new electric devices for pasteurizing soils. New York (Cornell) Agr.
Exp. Sta. Bui. 731: 1-38.
1955. Disinfestation of soil by heat, flooding and fumigation. Bot. Rev. 21: 189-250
Newhall, A. G., C. Chupp, and C. E. F. Guterman
1940. Soil treatments for the control of diseases in the greenhouse and the seedbed. New York
(Cornell) Agr. Ext. Bui. 217: 1-58.
Patten, H. E.
1909. Heat transference in soils. U. S. Dept. Agr. Bur. Soils Bui. 59: 1-54.
Penman, H. L.
1940. Gas and vapour movements in the soil. II. The diffusion of carbon dioxide through porous
solids. Jour. Agr. Sci. 30: 570-81.
Perkins, J. J.
1954. Bacteriological and surgical sterilization by heat. In: G. F. Reddish. Antiseptics,
disinfectants, fungicides, and chemical and physical sterilization, p. 655-82. Lea and
Febiger, Philadelphia, Penn.
Precision Scientific Co.
1955. Dry heat sterilization. Precision Scientific Co. (Chicago, 111.) Bui. 337: 1-15.
Rudd, W. N.
1893. Killing grubs in soil. Amer. Florist (Chicago, 111.) 9 (278) : 171.
Schwarz, A. R. VON
1879. Vergleichende Versuche iiber die physikalischen Eigenschaften verschiedener Boden-
arten. Forsch. Gebiete Agr.-Phys. 2: 164-69.
Senner, A. H.
1934. Application of steam in the sterilization of soils. U. S. Dept. Agr. Tech. Bui. 443: 1-20.
Stone, G. E., and R. E. Smith
1898. Nematode worms. Massachusetts Agr. Exp. Sta. Bui. 55: 44-65.
Stout, G. L., and W. F. Hiltabrand
1954. Approved treatment and handling methods for vegetable plants grown in flats to be
shipped under Intercounty Nursery Stock Certificates. California Dept. Agr. Mimeo.
3063-4. 1 p.
Tavernetti, J. R.
1950. Heat is best for soil sterilization. Pacific Coast Nurseryman 9 (8) : 14, 32.
Togashi, K.
1949. Biological characters of plant pathogens temperature relations. 478 p. Meibundo Co.,
Tokyo, Japan.
[291]
Zimmerman, 0. T., and I. Lavine
1945. Psychrometric tables and charts. 162 p. Industrial Research Service, Dover, New
Hampshire.
Section 10
Anonymous
1940. Formaldehyde and steam mixture for sterilizing greenhouse soil. DuPont Agr. News
Letter 8 (5) : 71-72.
1952. Steam sterilizing soil. Ohio Florists Assoc. Bui. No. 276: 2-3.
1953. Steam soil sterilizer firm names national distributor. Pacific Coast Nurseryman 12 (5) :
46-47.
1954. Soil handling. Grower Talks (West Chicago, 111.) 18 (4) : 26.
1955. [Portable steam generator.] Grower Talks (West Chicago, 111.) 19 (8) : 22.
1956. Mr. Jackson improves his steam traveller. The Grower (London) 46: 991, 993, 995.
1957. Growers see a steam plough from Holland. The Grower (London) 47: 97.
Ball, G. K.
1942. Sterilizing. Why and how? 26 p. Geo. J. Ball Inc., West Chicago, 111.
Ball, V.
1953. Modern methods of steaming soils. Grower Talks (West Chicago, 111.) 17 (4) : 1-7;
(5) : 1-7.
1954. Steaming aster cloth houses. Grower Talks (West Chicago, 111.) 17 (10) : 18-19.
1955. Steam rake sterilizing. Grower Talks (West Chicago, 111.) 18 (10) : 21-24.
Beachley, K. G.
1937. Combining heat and formaldehyde for soil treatment. Pennsylvania Agr. Exp. Sta. Bui.
348: 1-19.
Bewl'ey, W. F.
1939. Practical soil sterilization with special reference to glasshouse crops. 3d ed. Brit. Min.
Agr. Fisheries Bui. 22: 1-29.
1948. Practical soil sterilization with special reference to glasshouse crops. 4th ed. Brit. Min.
Agr. Fisheries Bui. 22: 1-22.
Brown, C. A. C, and P. Wakeford
1947. Electrical soil sterilization by immersion heaters. Brit. Elect. Allied Indus. Res. Assoc.
Tech. Rept. W/T 14: 1-17.
California Department of Agriculture, Bureau of Entomology and Plant Quarantine
1944. An inexpensive soil pasteurizing equipment. California Dept. Agr. Nursery Pest Control
Lflt. A-l: 1-3.
Canham, A. E.
1951. Electrode soil sterilizing. (Preliminary report.) Brit. Elect. Allied Indus. Res. Assoc.
Tech. Rept. W/T 21: 1-11.
COATES, W.
1954. New device for steam sterilising soil. The Grower (London) 42 (26) : 1247.
Dimock, A. W., and K. Post
1944. An efficient, labor-saving method of steaming soil. New York (Cornell) Agr. Ext. Bui.
635: 1-7.
Fosler, G. M.
1950. An efficient steam sterilizing box. Illinois Agr. Ext. Serv., Rept. from Hort., Flower
Growing No. 9 : 1-2.
Hansen, A.
1953-54. Dampning. Gartnertidende 18 (6) : 1 p.; 19 (1) : 1 p.
Hardy and Dillon, Inc.
1953. H and D electric heater assembly for soil sterilizers. 4 p. Hardy and Dillon, Inc., Boston,
Mass.
Johnson, J.
1930. Steam sterilization of soil for tobacco and other crops. U. S. Dept. Agr. Farmers' Bui.
1629: 1-13.
Lawrence, W. J. C.
1956. Soil sterilization. 171 p. George Allen and Unwin Ltd., London, England.
Lawrence, W. J. C, and A. C. Hunt
1955. The John [nnes high rate soil steriliser. John Innes Hort. Inst. Lflt. 13: 1-10.
| 292 ]
Lawrence, W. J. C, and J. Newell
1950. Seed and potting composts, with special reference to soil sterilization. 4th ed. 166 p.
George Allen and Unwin Ltd., London, England.
Morris, L. G.
1953. How to steam sterilise your casing soil. Mushroom Grow. Assoc. (Yaxley, England)
Bui. 45: 3 p.
1954. The steam sterilising of soil. The application of research to practice. Brit. Nat'l Inst.
Agr. Engin. Rept. 24: 1-22.
Newhall, A. G.
1930. Control of root>knot nematode in greenhouses. Ohio Agr. Exp. Sta. Bui. 451: 1-60.
1940. Experiments with new electric devices for pasteurizing soils. New York (Cornell) Agr.
Exp. Sta. Bui. 731: 1-38.
1953. How large a generator is needed to steam your soil. New York State Flower Growers
Bui. No. 91: 12.
Newhall, A. G., C. Chupp, and C. E. F. Guterman
1940. Soil treatments for the control of diseases in the greenhouse and the seedbed. New
York (Cornell) Agr. Exp. Sta. Bui. 217 (rev.) : 1-58.
Newhall, A. G., and W. T. Schroeder
1951. New flash-flame soil pasteurizer. New York (Cornell) Agr. Exp. Sta. Bui. 875: 1-19.
Peterson, M. L.
1942. An inexpensive soil sterilizer. Amer. Soc. Agron. Jour. 34: 674-76.
Roistacher, C. N., and K. F. Baker
1956. An inexpensive multipurpose soil steamer. Phytopathology 46: 329-33.
Roll-Hansen, J.
1949. Damping av jord. 68 p. A/L Norsk Gartnerforenings Forlag, Oslo, Norway.
Rudd, W. N.
1893. Killing grubs in soil. Amer. Florist (Chicago, 111.) 9 (278) : 171.
Schmitz, S. S.
1954. Steam sterilizing at lower cost. Florists' Rev. 114 (2961) : 19, 45.
Seeley, J. G.
1954. Steam sterilization of greenhouse soils. Pennsylvania Flower Growers Bui. No. 39 : 1-6.
Senner, A. H.
1934. Application of steam* in the sterilization of soils. U. S. Dept. Agr. Tech. Bui. 443: 1-20.
Tarrant Mfg. Co.
1955. Roto-therm soil pasteurizer. 2 p. Tarrant Mfg. Co., Saratoga Springs, N.Y
Tavernetti, J. R.
1935. Characteristics of the resistance type soil sterilizer. Agr. Engineering (St. Joseph, Mich.)
16: 271-74.
1942. A continuous soil pasteurizer. Agr. Engineering (St. Joseph, Mich.) 23: 255-56, 261.
Thomas, C. A.
1954. Some greenhouse soil pests and their control — nematodes. Pennsylvania Flower Growers
Bui. No. 47: 1-5,8.
Webrer, R.
1956. Mr. Jackson's soil steamer keeps on moving. The Grower (London) 45: 208-9.
Section 1 1
Hamner, O. H., and F. C. Amstutz
1955. Apparatus for more rapid vaporization of methyl bromide. Down to Earth (Midland,
Mich.) 11 (2): 11-13.
Jefferson, R. N., and A. E. Pritchard
1956. Pest control guide for California floricultural crops. California Agr. Ext. Serv. Lflt.
66: 1-11.
Kendrick, J. B., Jr., and G. A. Zentmyer
1957. Recent advances in control of soil fungi. In: Advances in pest control 1: 219-75. Inter-
science Publishers, Inc., New York, N.Y.
Lear, B.
1951. Use of methyl bromide and other volatile chemicals for soil fumigation. New York
(Cornell) Agr. Exp. Sta. Mem. 303: 1^8.
[293]
Lear, B., and W. F. Mai
1952. Methyl bromide for disinfesting burlap bags and machinery to help prevent spread of
golden nematode of potatoes. Phytopathology 42: 489-92.
Martin, W. J., N. L. Horn, and J. A. Cox
1955. Fumigation of bell pepper seed beds for controlling damping-off caused by Rhizoctonia
solani. Plant Dis. Reptr. 39: 678-81.
Munnecke, D. E., and J. Ferguson
1953. Methyl bromide for nursery soil fumigation. Phytopathology 43: 375-77.
Munnecke, D. E., and D. L. Lindgren
1954. Chemical measurements of methyl bromide concentration in relation to kill of fungi
and nematodes in nursery soil. Phytopathology 44: 605-6.
Newhall, A. G., and B. Lear
1948. Soil fumigation for nematode and disease control. New York (Cornell) Agr. Exp. Sta.
Bui. 850: 1-32.
Pritchard, A. E.
1949. California greenhouse pests and their control. California Agr. Exp. Sta. Bui. 713: 1-72.
Sciaroni, R. H.
1955. Terraclor for Rhizoctonia disease of carnation. California Agr. Ext. Serv., Alameda and
San Mateo Counties, Flower Notes No. 18 : 5.
Sciaroni, R. H., and R. D. Raabe
1955. Rhizoctonia disease control in carnations with PCNB. California Agr. Ext. Serv., Alameda
and San Mateo Counties, Flower Notes No. 16 : 6.
Stark, F. L., Jr.
1948. Investigations of chloropicrin as a soil fumigant. New York (Cornell) Agr. Exp. Sta.
Mem. 278: 1-61.
Section 12
Baker, K. F., and F. D. Heald
1934. Investigations on methods of control of the blue-mold decay of apples. Washington Agr.
Exp. Sta. Bui. 304: 1-32.
Huber, G. A.
1935. The use of sodium hypochlorite solutions as disinfecting agents. Better Fruit (Portland,
Ore.) 29 (12) : 5-6.
Klotz, L. J., and T. A. DeWolfe
1952. Steam sterilization of citrus field and storage boxes. Citrus Leaves 32 (12) : 20, 35.
Lear, B., and W. F. Mai
1952. Methyl bromide for disinfesting burlap bags and machinery to help prevent spread of
golden nematode of potatoes. Phytopathology 42: 489-92.
Roistacher, C. N.
1952a. Methods used in sterilizing nursery flats. Pacific Coast Nurseryman 11 (5) : 17, 34-36.
19526. Phytotoxicity of formaldehyde residue on flats. Phytopathology 42: 171-72.
Roistacher, C. N., and K. F. Baker
1954. Disinfesting action of wood preservatives on plant containers. Phytopathology 44: 65-69.
Wellman, R. H., and F. D. Heald
1938. Steam sterilization of apple boxes for blue mold. Washington Agr. Exp. Sta. Bui.
357: 1-16.
Section 1 3
Baker, K. F.
1948. The significance of disease-free seed and propagating material. Florists' Exch. 110
(9) : 21, 30, 58-59.
1952. A problem of seedsmen and flower growers — seed-borne parasites. Seed World 70 (11) :
38, 40, 44, 46-47.
1956. Development and production of pathogen-free seed of three ornamental plants. Plant Dis.
Reptr. Suppl. 238: 68-71.
BAKER, K. F., and P. A. CHANDLER
1956. Development and product inn of pathogen-free propagative material of foliage and suc-
culenl plants. Plant Dis. Reptr. Suppl. 238: 88 90
| 2<ri |
Baker, K. F., and K. Cummings
1943. Control of Pythium root rot of Aloe variegata by hot-water treatment. Phytopathology
33: 736-38.
Baker, K. F., and L. H. Davis
1950. Some diseases of ornamental plants in California caused by species of Alternaria and
Stemphylium. Plant Dis. Reptr. 34: 403-13.
Baker, K. F., and W. C. Snyder
1950. Plant diseases. Restrictive effect of California climate on some vegetable, flower, grain
diseases. California Agr. 4 (8) : 3, 15-16.
Brierley, P., and C. J. Olson
1956. Development and production of virus-free chrysanthemum propagative material. Plant
Dis. Reptr. Suppl. 238: 63-67.
Chandler, P. A.
1953. How to avoid diseases in plants and containers. Pacific Coast Nurseryman 12 (6) :
15-16, 44-45.
Chitwood, B. G.
1956. Root nematode problems in roses. Plant News (Blue Point, N.Y.) 6 (2) : 1.
Courtney, W. D., E. P. Breakey, and L. L. Stitt
1947. Hot-water tanks for treating bulbs and other plant materials. Washington Agr. Exp.
Sta. Pop. Bui. 184: 1-16.
Davis, L. H.
1953. Black cane rot of Syngonium auritum. (Abs.) Phytopathology 43: 586.
Dimock, A. W.
1943. Coming up-to-date on Verticillium wilt and Septoria leafspot of chrysanthemums.
Chrysanth. Soc. Amer. Bui. 11 (1) : 3-10.
1956. Production of chrysanthemum propagating material free of certain major pathogens.
Plant Dis. Reptr. Suppl. 238: 59-62.
Dimock, A. W., and K. F. Baker
1944. Hot-water treatment for control of Phytophthora root rot of calla. Phytopathology 34:
979-81.
Durbin, R. D.
1956. Hot-water seed treatment for control of a root rot complex of Strelitzia reginae. Plant
Dis. Reptr. 40: 1116.
Gasiorkiewicz, E. C, and C. J. Olson
1956. Progress in the development and production of virus-free carnation varieties. Plant Dis.
Reptr. Suppl. 238: 77-80.
Hansen, H. N., and W. C. Snyder
1947. Gaseous sterilization of biological materials for use as culture media. Phytopathology
37: 369-71.
Holmes, F. O.
1955. Elimination of spotted wilt from dahlias by propagation of tip cuttings. Phytopathology
45: 224-26.
1956a. Elimination of foliage spotting from sweetpotato. Phytopathology 46: 502-4.
19566. Elimination of aspermy virus from the Nightingale chrysanthemum. Phytopathology
46: 599-600.
Hughes, C. G.
1954. The eradication of sugar-cane diseases in Queensland. Fifth Commonwealth Mycol.
Conf. Rept., p. 59-64. Commonwealth Mycol. Inst., Kew, England.
Kendrick, J. B., Sr., and K. F. Baker
1942. Bacterial blight of garden stocks and its control by hot-water seed treatment. California
Agr. Exp. Sta. Bui. 665: 1-23.
Martin, C.
1954. Recherches sur les maladies a virus du dahlia. Ann. Epiphyties 5: 63-78.
Miller, P. W.
1954. Inactivation of non-persistent viruses in strawberry plants by hot-air treatment. Plant
Dis. Reptr. 38: 827-31.
MUNNECKE, D. E.
1956. Development and production of pathogen-free geranium propagative material. Plant Dis.
Reptr. Suppl. 238: 93-95.
[295]
Norms, D. 0.
1954. Development of a virus-free stock of Green Mountain potato by treatment with malachite
green. Austral. Jour. Agr. Res. 5: 658-63.
Quak, F.
1957. Meristeemcultuur, gecombineerd met warmtebehandelung, voor het verkrijgen van
virusvrije anjerplanten. Tijdschr. Plantenziekt. 63: 13-14.
Snyder, W. C, and H. N. Hansen
1947. Advantages of natural media and environments in the culture of fungi. Phytopathology
37: 420-21.
Tammen, J., R. R. Baker, and W. D. Holley
1956. Control of carnation diseases through the cultured-cutting technique. Plant Dis. Reptr.
Suppl. 238: 72-76.
Vaughan, E. K.
1956. A method for eliminating the red-stele fungus from valuable strawberry stocks. Phy-
topathology 46: 235-36.
Watson, R. D., L. Coltrin, and R. Rorinson
1951. The evaluation of materials for heat treatment of peas and beans. Plant Dis. Reptr. 35:
542^4.
West, E.
1942, 1943. Host relations and factors influencing the growth and parasitism of Sclerotium rolfsii
Sacc. Florida Agr. Exp. Sta. Ann. Rept. 1942: 93-94; 1943: 83-84.
Wilhelm, S., and R. D. Raare
1956. Culture-indexing of budwood to provide Verticillium-free greenhouse roses. Plant Dis.
Reptr. Suppl. 238: 85-87.
Young, R. A.
1954. Dissemination of plant pathogens on nursery and ornamental plants. Plant Dis. Reptr.
38: 417-20.
Section 14
Ark, P. A.
1937. Little-leaf or rosette of fruit trees. VII. Soil microflora and little-leaf or rosette disease.
Amer. Soc. Hort. Sci. Proc. 34: 216-21.
Ferguson, J.
1953. The effect of soil treatment on beneficial soil organisms. Pacific Coast Nurseryman 12
(7) : 15, 48.
Gerretsen, F. C.
1937. Manganese deficiency of oats and its relation to soil bacteria. Ann. Bot. n. s. 1: 207-38.
1948. The influence of microorganisms on the phosphate intake by the plant. Plant and Soil
1: 51-81.
Katznelson, H., A. G. Lochhead, and M. I. Timonin
1948. Soil microorganisms and the rhizosphere. Bot. Rev. 14: 543-87.
Martin, J. P., and J. O. Ervin
1952. Soil organisms — fact and fiction. Western Grower and Shipper 23 (6) : 30-32, 34-36,
38-39.
Meiklejohn, J.
1953. The nitrifying bacteria: a review. Jour. Soil Sci. 4: 59-68.
Nightingale, G. T.
1937, 1948. The nitrogen nutrition of green plants. Bot. Rev. 3: 85-174; 14: 185-221.
Waksman, S. A.
1932. Principles of soil microbiology. 2d ed. 894 p. Williams and Wilkins Co., Baltimore, Md.
1952. Soil microbiology. 356 p. John Wiley and Sons, Inc., New York, N.Y
Waksman, S. A., and R. L. Starkey
1931. The soil and the microbe. 260 p. John Wiley and Sons, Inc., New York, N.Y.
Section 15
Ark, P. A.
1937. Variability in the fire-blight organism, Erwinia amylovora. Phytopathology 27: 1-28.
Baker, K. F.
1917. Seed transmission of Rhizortonia solani in relation to control of seedling damping-off.
Phytopathology 37: 912-24.
L953. I'Hsariuni wilt of China aster. In: Plant diseases. U. S. Depl. Agr. Yearbk. 1953: 572-77.
[ 296 1
Chitwood, B. G.
1949. "Root-knot nematodes" — part 1. A revision of the genus Meloidogyne Goeldi, 1837.
Helminth. Soc. Wash. Proc. 16: 90-104.
Ferguson, J., and B. B. Markley
1955. The masking of soil treatment effects from use of contaminated planting stock (Abs.).
Phytopathology 45: 693.
Goodey, T.
1933. Plant parasitic nematodes and the diseases they cause. 306 p. E. P. Dutton and Co.,
Inc., New York, N.Y.
Holdeman, Q. L., and T. W. Graham
1954. Effect of the sting nematode on expression of Fusarium wilt in cotton. Phytopathology
44: 683-85.
Kendrick, J. B., Jr.
1951. The influence of temperature upon the incidence of Rhizoctonia root rot of lima beans.
(Abs.) Phytopathology 41: 20.
Lacey, M. S.
1939. Studies on a bacterium associated with leafy galls, fasciations and "cauliflower" dis-
ease of various plants. Part III. Further isolations, inoculation experiments and
cultural studies. Ann. Appl. Biol. 26: 262-78.
McCubbin, W. A.
1954. The plant quarantine problem. 255 p. Ejnar Munksgaard, Copenhagen, Denmark.
Rawlings, R. E.
1940. Observations on the cultural and pathogenic habits of Thielaviopsis basicola (Berk,
and Br.) Ferraris. Missouri Bot. Gard. Ann. 27: 561-98.
Roth, L. F., and A. J. Riker
1943. Life history and distribution of Pythium and Rhizoctonia in relation to damping-off of
red pine seedlings. Jour. Agr. Res. 67: 129-48.
Sanford, G. B.
1938. Studies on Rhizoctonia solani Kiihn. III. Racial differences in pathogenicity. Canad. Jour.
Res., Sec. C, 16: 53-64.
Sasser, J. N.
1952. Identification of root-knot nematodes {Meloidogyne spp.) by host reactions. Plant Dis.
Reptr. 36: 84-86.
Sasser, J. N., H. N. Powers, Jr., and G. B. Lucas
1953. The effect of root knot nematodes {Meloidogyne spp.) on the expression of black shank
resistance in tobacco. (Abs.) Phytopathology 43: 483.
Snyder, W. C., and H. N. Hansen
1940. The species concept in Fusarium. Amer. Jour. Bot. 27: 64—67.
Stewart, R. N., and A. F. Schindler
1956. The effect of some ectoparasitic and endoparasitic nematodes on the expression of
bacterial wilt in carnations. Phytopathology 46: 219-22.
Stover, R. H.
1950. The black rootrot disease of tobacco. I. Studies on the causal organism Thielaviopsis
basicola. II. Physiologic specialization of Thielaviopsis basicola on Nicotiana tabacum.
Canad. Jour. Res. Sec. C, 28: 445-70; 726-38.
Tarjan, A. C.
1952. Pathogenic behavior of certain root-knot nematodes, Meloidogyne spp. on snapdragon,
Antirrhinum majus L. Phytopathology 42: 637-41.
Tucker, C. M.
1931. Taxonomy of the genus Phytophthora de Bary. Missouri Agr. Exp. Sta. Res. Bui. 153:
1-208.
Wilhelm, S., and R. D. Raabe
1956. Culture-indexing of budwood to provide Verticillium-free greenhouse roses. Plant Dis.
Reptr. Suppl. 238: 85-87.
WORMALD, H.
- 1945. Physiologic races of the crown gall organism in Britain. Brit. Mycol. Soc. Trans. 28:
134-46.
[297]
Section 17
Baker, K. F.
1948. Nursery seedlings. Improved methods of production with control of damping-off disease.
Pacific Coast Nurseryman 7 (11) : 9, 28-29, cover.
Ball, V.
1953. Erdprinz. Grower Talks (West Chicago, 111.) 16 (10) : 14.
Connelly, J. R.
1943. Technique of production processes. 430 p. McGraw-Hill Book Co., Inc., New York, N.Y.
Harrington, C. C.
1952. Materials handling manual. 434 p. Conover-Mast Publ., Inc., New York, N.Y.
Hetzel, F. V., and R. K. Albright
1941. Belt conveyors and belt elevators. 439 p. John Wiley and Sons, Inc., New York, N.Y.
Hudson, W. G.
1954. Conveyors and related equipment. 3d ed. 524 p. John Wiley and Sons, Inc., New York,
N.Y.
Immer, J. R.
1953. Materials handling. 591 p. McGraw-Hill Book Co., Inc., New York, N.Y.
KOSHKIN, S. J.
1932. Modern materials handling. 488 p. John Wiley and Sons, Inc., New York, N.Y.
MUTHER, R.
1944. Production-line technique. 320 p. McGraw-Hill Book Co., Inc., New York, N.Y.
Staniar, W.
1950. Plant engineering handbook. 2,007 p. McGraw-Hill Book Co., Inc., New York, N.Y.
Stocker, H. E.
1951. Materials handling. Principles, equipment, and methods. 2d ed. 330 p. Prentice-Hall,
Inc., New York, N.Y.
GLOSSARY OF TERMS, AND SOME COMPUTATION METHODS
Aerobic — Living or active only in the presence of oxygen.
Anaerobic — Living or active in the absence of free oxygen.
Antibiotic — A chemical substance produced by an organism which inhibits the de-
velopment of a microorganism.
Bacterium — A microscopic unicellular plant that lacks chlorophyll and reproduces
by dividing into two parts; some cells may develop into resistant spores.
Boiler horsepower — Unit of boiler capacity; different from mechanical horse-
power. Is equal to heat required to convert 34.5 pounds of water at 212° F into
steam. Since it requires 970.3 B.t.u. per pound to convert water to steam, 1
horsepower equals 33,475 B.t.u. The term is indefinite as commercially used
because it is determined by measuring the cross-sectional area of actual heat
exchange between the source of heat and the water, without reference to ef-
ficiency or design. Boiler capacity is best expressed as pounds of steam gen-
erated per hour. For calculated conversion to boiler horsepower see table 14.
Boiler output of steam — Roughly calculated for small boilers by injecting the
steam into a weighed container of cold water for a measured time (water must
not be heated to point of vaporizing), and the container then reweighed. The
difference represents the pounds of steam delivered to the container during the
given number of minutes and may easily be converted to pounds per hour.
B.t.u. (British thermal unit) — Unit for quantity of heat; amount of heat required
to raise the temperature of 1 pound of water 1 degree F.
B.t.u. requirement for heating soil — See Section 8, "Cost of Steaming Soil,
Heal Requirements."
[298]
Buffering capacity — The relative ability of a soil solution to resist change; as
used in this manual it refers to pH. It is also used in a biological sense to in-
dicate the ability of a population of soil microorganisms to resist change.
Conductance — The reciprocal of the resistance (in ohms) of an electrolyte to the
passage of electrical current. The greater the salt content of the water, the
greater the conductance. Measured by a Wheatstone bridge (Solubridge) and
expressed as millimhos per cm (EC x 103) or mhos per cm x 100,000 (EC x
105).
Efficiency of boiler — May be approximated (in per cent) by multiplying the heat-
ing value of the fuel in B.t.u. (Sec. 10) by the quantity used per hour, and
dividing this figure into the product of the output of steam in pounds per hour
(see sees. 9 and 10, and "Boiler output of steam," above) and 1,150 B.t.u.
(fig. 77). Multiply the result by 100 to convert to percentage.
Efficiency of soil steaming operation — Multiply 970 B.t.u. plus half the dif-
ference between 212° F and the initial soil temperature (fig. 77) by the pounds
of steam necessary to heat the volume of soil to 212° (see Sec. 9 and "Steam
delivered to treatment site," below) . Divide this figure by the product of the
B.t.u. required to heat 1 cubic foot of soil (see Sec. 8, "Heat Requirements")
and the cubic feet of soil treated. This will provide the approximate efficiency.
The calculation may be stated as a mathematical formula thus:
„_„„ 212° F- initial soil temperature "1 „ , , nnn.
970 B.t.u. -f x lbs. steam required to heat to 212
B.t.u. required per cu. ft. x cu. ft. of soil treated
Multiply the result by 100 to convert to percentage.
Efficiency of steam distribution system — The pounds of steam per hour at the
boiler, minus the pounds of steam per hour at the treatment site, gives the
pounds per hour lost in distribution. This figure, divided by the pounds of
steam at the boiler and multiplied by 100, gives the percentage loss in distribu-
tion.
Fungistatic — Preventing growth of a fungus without killing it. Fungicidal is killing
the fungus.
Fungus — A primitive plant that lacks chlorophyll and is undifferentiated into root,
stem, or leaves; it reproduces by spores.
Heat capacity — See "Specific heat," below.
Heat conductivity — Rate of heat transfer by conduction through a material; usu-
ally expressed as calories per second per sq. cm for 1 cm thickness and 1 degree C
temperature differential. Comparative heat conductivities of some materials are :
water 0.0014, peat soil 0.00015, cork 0.0001, air 0.00006; most dry soils are of
the order 0.0007, increasing with moisture content up to about that of water.
Heat requirements — Dry soil requires about 1.200 B.t.u. per cubic foot per 100
degrees F of temperature rise. Soil moisture requires about 60 B.t.u. per 1 per
cent of water by weight for each 100 degrees F of temperature rise.
Host — A plant that is or may be attacked by a parasite or virus.
Infect, infection — The process by which a parasite gains entrance and becomes
established in the host.
Infest — To contaminate with microorganisms without infection or parasitism. Thus
a host may be infested or infected, whereas a nonliving object can only be in-
fested.
[299]
Inoculum potential — The relative quantity of a parasite in the environment of
the plant; interaction of inoculum potential, environment, virulence of the
strain, and host susceptibility determine the incidence of a disease.
Kilowatt-hour (K.w.h.) — Unit of electrical power or energy consumption;
amount of energy developed by 1 kilowatt per hour, equal to 3,411 B.t.u. or
roughly 1/10 boiler horsepower. For calculated conversion to boiler horse-
power see table 14.
Mycelium — The threadlike vegetative structure of a fungus.
Nematode — Minute wormlike animal; some types feed on or in plants.
Osmotic pressure — The negative pressure that influences the rate of diffusion of
water through a semipermeable membrane such as a cell wall.
Parasite — An organism that lives in or on, and obtains its nutrients from, a host
plant.
Pathogen — An organism or virus capable of causing disease in a host plant.
Pound of steam — Quantity of steam produced by evaporating 1 pound of water;
970 B.t.u. per pound are required to evaporate it, and the same number
are available to heat soil to 212° F as it condenses.
Retardant or antagonistic microorganisms — Microorganisms which delay
growth of, or disease production by, other microorganisms. This effect may be
brought about by (1) competing with other microorganisms for conditions
essential for growth, (2) parasitizing them, or (3) exerting an antibiotic effect
on them.
Rogue — To remove diseased plants from a crop, usually to obtain disease-free stock.
Saline soil — A soil containing soluble salts in such quantities that they interfere
with the growth of a crop plant. This is distinguished from alkali soils, which
contain sufficient exchangeable sodium to interfere with the growth of a crop
plant. A soil may be saline, nonsaline-alkali, or saline-alkali. Alkali soil is
distinct from alkaline soil, which has a pH reaction above neutrality and may
or may not be an alkali soil.
Salinity measurement — Conductance is measured by California nurserymen with
Solubridge equipment. Either the RD-26 or the RD-15 may be used, the latter
giving scale readings 100 times the former. This can be converted to approxi-
mate ppm by multiplying the RD-26 reading by 650 and the RD-15 by 6.5.
Saprophyte — An organism that obtains its nutrients from nonliving organic
matter.
Saturated steam — Steam still in contact with the water from which it was formed.
Almost all commercial steam used for soil treatment is of this type, and still
contains water droplets. It is of two kinds: (1) Low pressure, "pressureless,"
or free-flowing steam expands freely through the lines until it condenses. Its
pressure usually is below 5 pounds per square inch and its temperature only
slightly above 212° F. (2) Steam that is not permitted to expand freely and de-
velops pressure; the temperature also rises.
Sclerotium — A compact, resistant, dormant mass of mycelium by which the fungus
survives unfavorable conditions.
Soil moisture — Usually determined by weighing a sample both before and after
water is driven off at 221 ° or 230° F. The weight of water lost, divided by the
dry weight, gives the moisture percentage by weight.
| 300 ]
Specific heat — Ratio of the heat capacity of a substance to that of water. The heat
capacity is the number of calories of heat necessary to raise the temperature of
1 gram of a substance 1 degree C. For purposes of comparison, the specific heat
of water is about 1.0, those of steam and wood about 0.5, those of dry air, dry
soil, and aluminum about 0.2, and that of steel about 0.1. Thus, it takes about
twice as many B.t.u. to heat 1 pound of water as 1 pound of steam, and about 5
times as many as for dry soil or air.
Spore — A reproductive body of fungi and bacteria by which they spread or survive
unfavorable conditions.
Steam delivered to treatment site — The same procedure as for "Boiler output
of steam," above, is carried out at the point of steam entry into the container.
The pounds per hour delivered at this point may then be computed.
Steam pressure — The pressure exerted per square inch of surface by the steam.
Water expands 1,600 times as it is converted to steam, building up pressure
in the confined area if not permitted to escape freely. This is measured in gauge
pressure per square inch. This is not related to the quantity (pounds per hour)
of steam, and only slightly to its efficiency in steaming soil. The temperature in-
creases with the pressure (fig. 77) .
Substrate — Material in or on which an organism grows or to which it is attached.
Superheated steam — Steam removed from its water source and heated, much as
air is warmed. Because water in the saturated steam evaporates on superheating,
this type of steam is dry. It transmits about 47 B.t.u. per 100 degrees F of super-
heat more than saturated steam.
Water mold — A primitive type of fungus (one of the Phycomycetes) that lives in
very moist soil; some are able to parasitize plants.
WEIGHTS AND MEASURES
1 bu. = 1.24 cu. ft.; 0.05 cu. yd.; 3 standard southern California flats.
1 cc (cubic centimeter) = 0.061 cu. in.; 0.034 fl. oz. ; 0.001 liter.
1 cu. ft. = 0.037 cu. yd. ; 0.804 bu. ; 28,317 cc ; 1,728 cu. in.
1 cu. yd. = 27 cu. ft.; 46,656 cu. in; 21.70 bu.; fills 60 standard southern California
flats (18 x 18 x 3 in.) with soil.
1 gal. of water = 231 cu. in. ; 0.13 cu. ft. ; 8.34 lb. ; 8 pints.
1 lb. of water (60° F) = 0.12 gal. ; 0.016 cu. ft. ; 27.71 cu. in.
1 lb. per cu. yd. - 1 lb. per 27 cu. ft.; 1 lb. per 21.7 bu.; 0.74 oz. per bu. ; 0.59 oz. per
cu. ft.; 3.6 grams per gal.
1 lb. = 453.6 grams; 16 oz.
1 ml (milliliter) = 1 cc (see above) .
1 oz. (avdp.) = 28.3 grams; 0.0625 lb.
1 oz. (fluid) = 29.6 cc or ml; 0.0625 pint; 2 tablespoons.
1 pint = 16 fl. oz.; 473.2 cc or ml; 0.125 gal.; 32 tablespoons.
[301]
SOURCES OF EQUIPMENT AND MATERIALS2
Boilers, package and flash type
Cleaver-Brooks Self-contained Boilers. Cleaver-Brooks Co., Milwaukee, Wis.
Cyclotherm Generator. Cyclotherm Division, U. S. Radiator Corp., Oswego 1, N.Y.
Francis Steam Generators (1%, 2%, 3%, 5, 8, 10, 15, 25, 40, 60 h.p.) Francis
Steam Generator Co., Inc., Bellflower, Calif.
Hypressure Steam Jenny. Metropolitan Greenhouse Mfg. Co., Brooklyn 37, N.Y.
Iron Horse Electric Steam Generator. North Bay Electric Works Inc., San Rafael,
Calif.
Sellers Immersion Steam Boilers. Sellers Engineering Co., Chicago 40, 111.
Steam-flo soil sterilizer. Rough Bros., Cincinnati 23, Ohio.
Steam Master steam generator. Lord and Burnham, Mt. Eden, Calif.
Boilers, regular, low or high pressure
There are many types, sizes, and makes available, both new and secondhand, that
can be used for soil steaming. For information on these consult a heating engi-
neer.
Fertilizing equipment
Proportioner. Smith Precision Fertilizer Injector. Smith Precision Products Co.,
1135 Mission St., South Pasadena, Calif.
Hot-water-treating equipment
Tanks. National Blower and Sheet Metal Co., 1129 St. Paul Ave., Tacoma 2, Wash.
Thermometer, chemical. 0° to 220° F, 12 in. -length, full immersion, nitrogen-filled.
Available: 1, 2.
Thermometer, precision grade, normal, 30° to 220° F in ^5° F subdivisions. For
calibrating and standardizing the above thermometers. Available: 1, 2.
Thermometer with expanded scale in critical range. Custom-made, with expanded
ranges available at 86° to 113°, 113° to 140°, or 104° to 131° F. N. V. Pieter-
man, Division of M. van Baaren, Den Haag, Netherlands.
Planting equipment
Erdprinz Planter. Imported by The Plant Products Corp., Blue Point, Long Island;
under test by Geo. J. Ball, Inc., West Chicago, 111.
Vacuum Plate Seed Planters. Ames Powercount Co., Brookings, South Dakota.
Planting machines for cans and pots. Oki Nursery, Perkins, Calif.
Soil-fumigation equipment
Aeron Cover (vinyl-coated nylon) . Expensive, but very durable. Available: 3, 4, 6.
Hand and machine injectors, etc. Available: 3, 4, 6.
Ultron Cover (polyvinyl chloride). Expensive, but very durable. Available: 3,
4,6.
Visqueen Cover (polyethylene). Cheapest, least durable covers; excellent for pur-
pose. Available: 3, 4, 6.
' Dealers supplying several items are listed numerically under Equipment Dealers at the end
of this section; numbers refer to these sources. Types of soil-steaming equipment refer to those
in Section 10. Materials and equipment mentioned by trade names in the text are listed, with
some sources where they were available when this manual was prepared. No endorsement of
these materials or sources is intended, nor is criticism implied of similar products or sources not
mentioned.
| 302 ]
Soil-steaming equipment
Aluminum pipe. Armco Drainage and Metal Products Co., Berkeley and Los An-
geles. Also see dealers in portable irrigation pipe.
Duratex Cover. American Associated Co., Red Bank, N.J.
Elliott Steam Soil Sterilizer. (Revolving screw, with steam generator; type 29).
Elliott Manufacturing Co., Fresno, Calif.
Fiberthin Cover (U. S. Rubber Co.). Colorado Tent and Awning Co., Denver 2.
Colo.
Hardy and Dillon Electric Heater Assembly. (Immersion heaters, type 14) . Hardy
and Dillon Co., Inc., Boston 8, Mass.
Pike's Peak Plastic Covering. Available: 5.
Porous canvas hose for Thomas Method. Available: 5.
Porto Portable Soil Sterilizer. (Mobile bin; type 2). Fairview Plant Farm, Janes-
ville, Wis.
Roto-therm Soil Pasteurizer. (Horizontal rotating drum, external flame, batch,
type 35) . Tarrant Mfg. Co., Saratoga Springs, N.Y.
Sisalkraft Paper Cover. Often available at lumberyards.
Snyder's Plastic Covering. M. L. Snyder and Son, Cincinnati 27, Ohio.
Steam box (types 4a, 4b). Fabricated on order by H. Ernest Ashton Plumbing
and Heating, 1707 S. Hoover St., Los Angeles 6, Calif.
Stericover (Goodyear Rubber Co.). Jednak Floral Co., Columbus 16, Ohio.
Steriltex and Sterilite. Dahm's Greenhouse and Garden Supplies, Des Plaines, 111.
Tarco Flash-flame Soil Sterilizer. (Rotating drum, with internal blow torch; type
30). Tarrant Mfg. Co., Saratoga Springs, N.Y.
Tempil Pellets. Available: 1, 2.
Tufedge Cover. Cleveland Cotton Products, Cleveland 14, Ohio.
Velon Fumicover (Firestone Rubber Co.). Industrial Fumigation Co.. Chicago.
111.
Visqueen. See "Soil-fumigation equipment," above.
Soil-testing equipment
Balance, Harvard trip, triple beam, 2,000-gram capacity. Available: 1, 2.
Biichner funnel filter, porcelain, 71- or 75-mm inside diameter. Available: 1, 2.
Centimeter rule. Available: 1, 2.
Filter flask, Erlenmeyer Pyrex heavy wall, with tubulation, 500 ml. Available:
1,2.
Filter paper, Whatman No. 50, 7-cm diam., hard. Available: 1, 2.
Filter pump, brass, to attach to water faucet. Available: 1, 2.
Funnel support, wood, supported at 2 ends, for 4 to 6 funnels. Available: 1. 2.
Graduated cylinder. 10-ml capacity. Available: 1, 2.
Hydrometer jar. Bouyoucos, graduated at 1,000 ml. Available: 1, 2.
Rubber tubing, pressure, Y^- and %e_m- inside diameters. Available: 1, 2.
Sieve, screen. Standard No. 35, 32-mesh or 0.5 mm. Available: 1, 2.
Soil hydrometer, Bouyoucos A. Available: 1, 2.
Solubridge RD-26, and Pipette Fill-type Conductivity Cell. Available: 1, 2.
[303 ]
Test tubes, Pyrex filtration, with side tabulation, 18- to 20-mm outside diameter.
Available: 1,2.
Test tubes, Pyrex, with rim, 150 mm long, 20-mm diameter. Available: 1, 2.
Thermometer (see above).
Equipment dealers
1. Braun Corp., 2260 E. 15th St., Los Angeles 21, Calif.
2. Braun-Knecht-Heiman Co., 1400 16th St., San Francisco 19, Calif.
3. Larvacide Products, Inc., 1515 S. 3rd St., San Francisco, Calif.
4. Neil A. Maclean Co., Inc., 184 S. Alvarado St., Los Angeles 57; 470 8th St.,
San Francisco 3, Calif.
5. Pike's Peak Greenhouses, Inc., Colorado Springs, Colo.
6. Service Chemical Supply Co., 4937 Telegraph Rd., Los Angeles 22, Calif.
SOURCES OF FUNGICIDES AND CHEMICALS3
Captan (Orthocide 406, Captan 50W). N-trichloromethylmercapto-4-cyclohexene-
1 :2 dicarboximide. Available: 7, 25.
Chloropicrin (Larvacide). Trichloronitromethane. Available: 13, 15, 22.
Copper naphthenate. Available: 4, 12.
DD mixture (Dowfume N, Shell D-D). Dichloropropene, dichloropropane mixture.
Available: 11,23.
Demeton (Systox). 0,0-diethyl O-2-ethylmercapto-ethyl phosphorothioate. Avail-
able: 6, 7, 8, 10, 14, 19, 20, 25.
Dieldrin. 1,2,3,4,10. 10-hexachloro-6, 7-epoxy-l,4,4a,5,6,7,8,8a octahydro-1, 4,5,8
dimethanonaphthalene. Available: 6, 7, 8, 10, 14, 19, 20, 25.
Distilled water. Available: 1, 2, 18.
Dura-K. Potash frit. Available: Glostex Chemicals Inc., 3056 Bandini Blvd., Los
Angeles 23, Calif.
Ethylene dibromide (EDB, Dowfume W40 and W85, Bromofume 40 and 85, E-D-
Bee). 1,2 dibromomethane. Available: 11.
Ferbam (Fermate, Karbam, Nu-leaf Black, Ferradow). Ferric dimethyldithio-
carbamate. Available: 8, 14, 17, 19.
Formaldehyde. Available: 4, 5, 6.
Malathion. S-(l :2-dicarbethoxyethyl-0,0-dimethyl phosphorodithioate) . Available:
6,7,8,10,14,19,20,25. . •
Methyl bromide, gaseous 100 per cent (mixtures containing 2 per cent chloropicrin
sold as MC-2, MBC Fumigant, Pestmaster Soil Fumigant). Available: 11, 13, 15,
22. The liquid form (Bromex, Edco MBX) is not sold in California for use on
nursery soils.
Nabam (Dithane D-14, Parzate Liquid, Ortho-Nabam) . Disodium ethylene bisdi-
thiocarbamate. Available: 7, 8, 14, 17, 19, 21.
'Sources of supply are listed numerically at the end of this section; numbers refer to these
sources. Most of the materials are also obtainable from local fungicide or insecticide companies.
Chemicals mentioned by trade names in the text are listed, with some sources where they were
available when ibis manual was prepared. No endorsement of these chemicals or sources is in-
tended, nor is criticism implied of similar products or sources not mentioned.
! 304 I
Nemagon. 1.2-dibromo-3-chloropropane. Available: 23.
Parathion. O.O-diethyl O-p-nitrophenyl phosphorothioate. Available: 6, 7, 14. 25.
PCNB (Mathieson 275. Terraclor I . Pentachloronitrobenzene. Available: 6, 16.
V
Potassium chloride. solution. Available: 9.
100
Puratized Agricultural Sprav. Phenvl mercury triethanolammonium lactate. Avail-
able: 20, 24.
Semesan. Hydroxymercuriochlorophenol. Available: 14, 17.
Sodium hypochlorite solution, approximately 5 per cent available chlorine. May be
obtained in small quantities at grocerv stores as Clorox. Purex, etc. Available:
4, 5.
Sodium oxalate. Available: 4, 5.
Sodium selenate (mixture with 2 per cent sodium selenate marketed as P-40).
Available: Plant Products Corp.. Blue Point, N.Y.
Stoddard solvent (Standard Thinner No. 350). Available: 3, 12.
Thiram (Arasan, Tersan ) . Tetramethylthiuram disulfide. Available: 14, 17.
Triton B-1956 Spreader. Available: 21.
Vapam (N-869). Sodium N-methyl dithiocarbamate dihydrate. Available: 25.
V-C 13. 0-2.4-dichlorophenyl O.O-diethyl phosphorothioate. Available: Virginia-
Carolina Chemical Corp.. Richmond 8. Ya.
Zineb ( Parzate. Dithane Z-78). Zinc ethvlene 6zsdithioearbamate. Available: 8, 14.
17, 19, 21.
Chemical dealers
1. Alhambra National Water Co., 2217 Revere Ave., San Francisco, Calif.
2. Arrowhead and Puritas, Inc., 1566 E. Washington Blvd., Los Angeles, Calif.
3. Bortz Oil Co.. 9423 Exposition Blvd., Los Angeles, Calif.
4. Braun Corp.. 2260 E. 15th St., Los Angeles 21, Calif.
5. Braun-Knecht-Heiman Co., 1400 16th St., San Francisco 19, Calif.
6. L. H. Butcher Co.. 3628 E. Olympic Blvd., Los Angeles; 15th and Vermont St.,
San Francisco, Calif.
7. California Spray-Chemical Corp., Lucas and Ortho W ay. Richmond, Calif.
8. A. L. Castle Seed Co., 248 View St.. Mountain View, Calif.
9. Central Scientific Co. of California, 6446 Telegraph Rd.. Los Angeles 22; 16
Beale St., San Francisco 5, Calif.
10. Chipman Chemical Co., Bay Road, East Palo Alto, Calif.
11. Dow Chemical Co.. 900 Wilshire Blvd.. Los Anseles: 350 Sansome St.. San
Francisco, Calif.
12. Harshaw Chemical Co., 3237 S. Garfield Ave., Los Angeles, Calif.
13. Larvacide Products. Inc.. 1515 S. 3rd St.. San Francisco. Calif.
14. Los Angeles Chemical Co.. 1960 Santa Fe. Los Angeles. Calif.
15. Neil A. Maclean Co., Inc., 184 S. Alvarado St.. Los Angeles 57: 470 8th St., San
Francisco 3, Calif.
16. Mathieson Chemical Corp., 7183 E. McKinley, Fresno, Calif.
17. McCrea Seed and Chemical Co.. Santa Barbara. Calif.
18. Mountain Spring W ater Co.. 226 S. Ave. 54. Los Angeles 42. Calif.
19. Mover Chemical Co., P. O. Box 945. San Jose. Calif.
[305]
20. Niagara Chemical Division of Food Machinery Corp., P. 0. Box 1589, Richmond,
Calif.; 206 Bassett St., San Jose, Calif.
21. Rohm and Haas Co., 1404 Franklin St., Oakland, Calif.
22. Service Chemical Supply Co., 4937 Telegraph Rd., Los Angeles 22, Calif.
23. Shell Chemical Co., 1008 W. 6th St., Los Angeles; 100 Bush St., San Francisco,
Calif.
24. James A. Southwick, c/o Food Machinery Corp., Riverside, Calif.
25. Stauffer Chemicals, 636 California St., San Francisco 8; 824 Wilshire Blvd.,
Los Angeles 14, Calif.
ACKNOWLEDGMENTS
A synthesis such as this, of information bordering on several fields, must draw
on the common reservoir of knowledge and experience. In numerous ways this
publication represents the accumulated experience of many people in various areas
of the world. Farm advisors and growers have helped check the validity of our con-
clusions in local practice, and have suggested modifications of them. To all who have
so generously assisted in these studies, both directly and through their published
papers, we are deeply grateful.
In addition to those specifically mentioned in the text, we are especially indebted
to M. W. Gardner, W. F. Hiltabrand, M. R. Huberty, H. J. Ishida, L. J. Klotz, B.
Lear, O. R. Lunt, J. P. Martin, A. O. Paulus, R. L. Perry, C. E. Scott, S. A. Sher,
W. C. Snyder, C. Tasche, J. R. Tavernetti, R. E. Weidner, and S. Wilhelm for
advice, encouragement, and assistance in the course of the work and preparation of
the manuscript. Mrs. L. H. Davis prepared the line drawings and R. D. Durbin the
graphs; B. B. Markley took some of the photographs. Mrs. Jane Simonsen, Mrs.
Mary Bogart, Mrs. Mary Falzone, and Mrs. Katharine Baker aided in the prepara-
tion of the manuscript for the printer.
The material in each section was prepared by the named authors, read and dis-
cussed by others of the group, and then revised. To this extent the information
represents the collective experience and concepts of the ten persons directly involved.
Final responsibility rests, however, with the authors of each section.
Submitted for publication June 10, 1955.
[306]
Acknowledgments, 306
Actinomycetes, 21, 238, 242, 245, 254
Adiantum (maidenhair fern), 215
Adobe soil, 86, 268
Adopting the U. C. system, 1-2, 27, 79, 263-64
Aeration of seedlings and damping-off, 43
Aeration of soil, 10, 60, 87-89, 98-99, 120, 121,
143, 259; relation to fnmigant diffusion,
142-43; to microorganisims, 121, 140, 244;
to organic-matter content, 98-99; to particle
size, 98-99; to percentage porosity, 87, 89,
143; to pore size, 143, 149; to steam move-
ment, 132-43, 149; to water content, 87-89;
to water movement, 65-67
Aerobic microorganisms, 244, 298
Aeron cover, for soil treatment, 302
African violet, see Saintpaulia
Aging, of seed, 21, 232; of soil to reduce tox-
icity, 10, 93, 95, 96
Aglaonema, 226
Aids in adopting the U. C. System, 1-2
Air, heat conductivity of, 299; specific heat of,
301
Air-borne spores, 46; unimportant in Rhi-
zoctonia and water molds, 5, 250
Aleurites (tung), 257
Alfalfa, Rhizoctonia on, 257
Algae, in soil, 21, 238, 241; on containers, 19,
211
Alkali, 300
Alkalinity, soil, 87, 300
Allerton and Ray soil mix, 94
Allium (onion), 258
Aloe, heat treatment, 139, 226-27; Pythium
root rot, 139,226-27
Alternaria, 218, 229, 233
Aluminum, 95; irrigation pipe, 129, 178, 195-
96, 303; specific heat of, 301
Aluminum sulfate, 76
Amaryllis, salinity injury, 58
Amino acids, 51, 108, 245
Ammonia, anhydrous, 112; aqua, 109, 112;
toxicity, 112; see also Ammonium
Ammonifiers, 239-40, 245-46
Ammonium, 105, 109, 126, 241, 243, 244, 245
conversion to nitrate, 109, 113, 116-20; pre-
vented by steaming, 113-14, 116-20
difficulty of leaching from soil, 95, 99, 109
effect of gypsum on, in soil, 10, 96, 109
injury to plants, 13, 14, 105, 109, 113, 252-
54
occurrence in field soils, 109, 246
release from organic nitrogen, 13, 14, 53, 95,
105, 115, 116-19; not prevented by steam-
ing, 113-14
retarded movement through soil, 14, 109,
122
INDEX1
role in soil toxicitv, 94-96, 199
toxicity, 9, 13-14, 79, 111-13, 121, 122, 199;
control by omitting organic nitrogen, 13,
115; control by prompt planting, 10, 95-
96; control by surface application of or-
ganic nitrogen, 14, 119; control by use of
nitrate fertilizers, 14, 111; control in pot-
ting-on, 119; possible cause of, 253-51;
sensitive plants, 13, 96, 111, 112, 115
See also Ammonia
Ammonium hydroxide, 112
Ammonium nitrate, 14, 53, 76, 78, 106, 1 12
Ammonium sulfate, 53, 76, 94, 106, 109, 111,
112
Anaerobic microorganisms, 244, 298
Anemone, mosaic, 21, 233
Anhydrous ammonia, 112
Animals, 245
Antagonistic organisms, 20, 21; balance in soil,
250-54; relation to U. C.-type mixes, 24, 35,
252-53; use to prevent soil contamination,
4, 20, 35, 250-53
Antibiotics, 255-56, 298; breakdown in soil,
34; produced by retardants, 24, 250-51, 300:
toxic to crops, 24, 25, 251, 253; use, 4, 34
Antirrhinum, see Snapdragon
Antiseptics, use, 4, 34
Aphelenchoides (foliar nematode), 20, 47, 139,
220, 232-33
Aphids, 235
Apium, see Celery
Apple, crown gall, 258; fire blight, see Fire
blight
Application of fertilizers
dry, 11, 14,76-77,79
inorganic, see Ammonium and Nitrate nitro-
gen
liquid, 14, 27, 76, 78, 79; proportioners for,
283, 302
organic, mixed in soil, 71-75, 122; on sur-
face, 13-14, 118-19, 121, 122
Aqua ammonia, 109, 112
Arachis (peanut), 259
Arasan (thiram), 19, 43, 207, 209, 305
Araucaria, Rhizoctonia top rot, 38, 220
Armillaria root rot, 135, 198; infecton from
plant parts, 260-61; obtaining stock free of,
220
Ascochyta, 233
Aseptic practices, 4, 34, 138
Aspermy virus, 221
Asphalt pavement, 41, 275
Aster, China, see China aster
Aster yellows virus, 232, 235
Attitude of grower toward change, 27, 265
Authors, iv
Autoclave (cannery retort) for soil steaming
Important discussions indicated in boldface type.
[307]
Autoclave, continued
(type 9), 16, 17, 25, 129, 151, 162, 164, 166,
174-75, 272; disadvantages, 129, 158; ther-
mal efficiency, 129, 158; unexpelled air, 132,
134, 147, 158', 174
Avena, 139
Avocado, Phytophthora root rot, 45, 258
Azalea, 12, 29, 69, 99, 120-21, 220; chlorosis,
107; Ovulinia flower blight, 21, 30, 232,
233, 234; Rhizoctonia decay of cuttings and
grafts, 38, 220; root injury from water, poor
aeration, 60, 99; salinity injury, 8, 60, 64
Bacteria, 15, 18, 21, 197, 216, 221-22, 237-38,
212, 245, 298; ammonifying, 239-40, 245-46,
254; lethal temperatures, 139; longevity,
243; nitrogen-fixing, 244-45; non-spore-
forming, 113, 139, 245; spore-forming, 113,
139, 245, 254, 298; sulfur, 246-47; varia-
bility of, 258
Bacterial blight of stock, longevity in soil, 261
Bacterial fasciation, 220, 233, 258
Bacterial leafspot of delphinium, 46, 47
Bacterial soft rot, 21, 35, 226-27, 233, 235;
spread by fungus flies, 227
Bacterial stem rot of geranium, 261; longevity
in soil, 261
Baking or burning of soil (type 17), 165, 166,
177
Balance in soil microorganisms, 21, 25, 238-
40, 250-54
Balanced soil steaming, 130, 150, 155, 159-60
Balled stock, 31
Bark, ground, 12, 80, 97, 98, 99; effect on soil
leachability, 65-67; phosphorus content,
99; potassium content, 99
Base exchange, definition, 99; of fine sand,
99; of loam and clay, 99; of peat moss, 99
Bean, treating fields, 205; Rhizoctonia on, 43,
205, 256
Bean straw, 268
Bedding plants, 29, 55, 84, 110, 126, 137, 203;
sales by months, 30; soil mixes, 12, 69, 72,
75, 79, 264-65; U. C. system for, 111, 113,
119,264-65
Beds, chemical treatment, 19, 200, 201, 203,
204; fertilizer schedule, 77, 80-81, 120; soil
mixes for, 80-81; steaming, 131, 133, 134,
162, 178-85, 192; U. C. system for, 12, 69,
80-81,268
Begonia, 79; heat treatment of tubers, 226;
root-knol nematode on, 226; salinity injury,
7, 9, 15, 53
Belonolaimus (sting nematode), 261
Benches, 126, 131, 210, 219, 250; chemical
treatmenl of, 19, 40, 200, 204, 213, 215; fer-
tilize] s< hedule lor, 77, 80-81, 120; soil mixes
for, 80-81; steaming, 40, 132, 134, 159, 178-
85, 211, 275; U. C. s\stem lor, 12, 69, 80-81,
268
Beneficial soil microorganisms, 238-40
Bicarbonate in water, 64
Bicvcle-wheel cart for pots, 281-82
Bin and potting bench, see Combined bin ana
potting bench
Bins, 134, 272-73
Biological control, see Controlled colonization
Bird-of-paradise plant (Strelitzia), 229
Biuret injury from urea fertilizers, 13, 14, 78,
79, 119
Black root rot (Thielaviopsis), 258
Black shank of cotton, 261
Blood meal, 13, 14, 53, 71-75, 76, 77, 79, 105,
106, 121; decomposition in soil, 115-19, 243
"Blow out" of steam from soil, 128, 149-50,
152-53, 159-60, 183; methods for prevent-
ing, 130-31, 155
Blow torch, bench disinfestation, 19, 211
Boiler, steam
capacity, 298
cost, calculation, 135-37
efficiency, thermal, 299
fuel for, 16, 162, 194-95
horsepower rating, vs. pounds of steam, 159-
60, 193-94, 298; vs. kilowatt-hours, 159,
300
modified hot-water boiler, 192
size required, 1, 132-33, 159-60, 193-94, 298;
calculation, 135-36
sources, 302
types, 159, 192, 302
Boron injury to plants, not prevented by
water deionizers, 64; related to water supply,
64; required by plants, 89, 106
Botrytis cinerea, 5, 46, 47 (fig. 33); aggravated
by salinity, 8, 9, 46, 55; lethal temperatures,
139; relation to Fusarium wilt in aster, 49-
50
Box-type soil heaters, with electric heating
element (type 14), 142, 165, 166, 176-77,
179, 195, 303; with electrodes (type 15), 165,
166, 177, 179, 195; with induction grid
type 16), 165, 166, 177, 195; see also Steam
box
Boxwood, heat treatment of plants, 226; root-
knot nematode on, 226
Brassica, see Cabbage and Mustard
Bromine toxicity from soil treatment, 10, 16,
17, 18, 124, 199,201, 206, 208
Broomrape, longevity in soil, 261
B.t.u., definition, 298
Buffering capacity, 299
Bulbs, 217, 255
Bur-clover seed, chemical resistance, 203; heat
resistance, 139
Buried perforated pipes for soil steaming
(type 20), Hi, 128, 131, 132, 138, 148, 150,
L52, 156, 165, 166, 178, 180-83, LSI, 194
Buried tiles lor soil steaming (type 22), 16,
131, 132, 1IH, 156, 165, 100, 178, 181, 183,
IS5
Bulla]) bags, treatment, 212
[308]
Bushel, 301
Butane, fuel for boilers, 16, 162, 187, 192, 194
Buttonweed (Malva), seed, chemical resistance,
203; seed, heat resistance, 139; spotted wilt,
235
Buxus, 226
Cabbage, 43
Cacti, 29, 37, 38
Caladium, bacterial soft rot, 226; heat treat-
ment of tubers, 226; Sclerotium rolfsii on,
139, 226
Calcium, 13, 64, 70, 95, 99, 106, 109, 110; avail-
ability affected by microorganisms, 237,
247; essential to plants, 89, 106
Calcium bicarbonate, 63
Calcium carbonate, 70, 72-75, 91, 101, 106
Calcium chloride, 65-67
Calcium nitrate, 13, 14, 76, 78, 105-6, 112,
119, 120, 265; starter solutions, 13, 14, 111-
12, 254
Calcium phosphate, 14
Calcium sulfate, 14, 96, 101, 106, 113, 115; see
also Gypsum
Calendula, 42, 215
California climate, effect on diseases, 29-30,
233; effect on salinity, 30; relative humidity,
233
California "native" plants, 37
Calla, 263; bacterial soft rot, 233, 234; chemi-
cal treatment of rhizomes, 20, 230; harden-
ing for heat treatment, 224; hot-water
treatment of rhizomes, 224, 229, 230; isola-
tion by growing in pots, 234-35; Phytoph-
thora root rot,- 20, 229, 230, 233, 234-35;
Rhizoctonia on, 233; spotted wilt, 21, 235
Callistephus, see China aster
Cal-mix, 93; see also U. C.-type soil mixes
Calsoil mix, 93; see also U. C.-type soil mixes
Camellia, 69; Rhizoctonia on, 43, 220; salinity
injury, 58; Sclerotinia flower blight, 21,
232, 233, 234; water mold root rot, 220
Canadian peat, see Peat, sphagnum
Can filler, 25, 26, 33, 166, 272-73, 280, 282,
302
Can nursery stock, 29, 31, 53, 126, 127, 137,
163, 168, 171, 173, 196, 201, 210, 211, 267;
fertilizer schedules for, 77, 80, 119; soil
mixes for, 69, 72, 80, 267
Canker, stem, 34
Cannery retort, see Autoclave
Cans of soil, steaming of, 142
Capsella, 139
Capsicum, see Pepper
Captan (Orthocide 406), 19, 43, 207, 209, 304
Carbohydrate-nitrogen status of plant, 253-
54; relation to damping-off, 5, 42
Carbon, 237, 242-44, 246; cycle, 246-47
Carbon dioxide, 6, 216, 241, 242; exchange
rate, soil to air, 143; in air, 87, 246; in soil,
87, 246, 259; relation to development of
Rhizoctonia, 259
Carbon/nitrogen ratios of organic matter, re-
lation to bacterial activity, 242-44; relation
to fungus activity, 242-44
Carbon tetrachloride, 223
Carbonic acid, 246; relation to available soil
nutrients, 216
Carborundum powder, 232
Carboxide, 216
Carnation, 7, 32, 111, 201, 203, 205, 20K, 209,
221, 234, 263; ammonium injury, 13, 111.
113; bacterial wilt, 35; bromine injury, 10,
16, 18, 95, 121, 199, 201, 206; cultured-cut-
ting technique with, 20, 221; mosaic, 234;
Rhizoctonia stem rot, 43, 205, 207, 208;
salinity injury, 7, 55, 58; U. C. system for,
268; virus diseases, 221, 232
Castanea (chestnut), 46
Castor-bean pomace, 13, 14, 76, 105, 115-19,
121
Cattleya, 90; salinity injury, 60
CBP 55 (chloro-bromo-propene), 199
Cedar, Port Orford, 46
Celcure wood preservative, 216
Celery, 25-26, 27, 111, 265-66; aging of seed,
21, 232; ammonium toxicity, 111; aster yel-
lows, 235; heat treatment of seed, 51; late
blight, 21, 51, 218, 226, 232; mosaic, 265
Cellulose, 241,251,254
Centipedes, lethal temperature, 139
Centralized soil service, 27
Ccratocystis fimbria ta, 229
Certification
of budwood, 31
of nursery stock in California, 31, 48-49,
129, 201; and soil treatment, 48, 129, 201;
and U. C. system, 49; "pinto tag," 48, 129,
201
Chalk, see Calcium carbonate
Chamaecyparis (Port Orford cedar), 46
Chelated iron, 107
Chemical components, of dry fertilizers, 76-
77: of liquid fertilizers, 76, 78; of U. C.-type
soil mixes, 69-76; see also Fertilizer ingre-
dients
Chemical residue in soil after treatment. 10.
98, 199; chloro-bromo-propene. 199; ethv-
lene dibromide, 199, 206; formaldehyde,
201, 212-13: kerosene, 190; methyl bromide,
10, 16, 17, 18, 124, 199, 202, 208
Chemical treatment of propagative material,
20, 230, 232, 236; effect of cracked seed
coats. 232; ineffective on internal parasites,
41-42, 230
Chemical treatment of soil (Section 11), 197-
209; also frontispiece. 1, 11, 22. 2:>. IS. 111.
123, 210, 252, 251, 2S0
aeration of treated soil, 199
best treated in containers, 48, 126-27
bulk soil, 273
[309]
Chemical treatment of soil, continued
causing salinity, 53
compared with steam, 1, 16, 18, 123-25, 210
correct dosage, importance, 22
cost, 197-98
dosage. 249-50
drenches, 19, 43, 48, 207, 209
effect on microorganisms, 18, 120, 248-50
effectiveness, 197, 201, 203, 204, 205
equipment for, 302
eradicative only in container soils, 197
ideal chemical, 197-98
importance of correct dosage, 207, 249-50
in containers, 201-2, 272
in "pinto tag" certification, 48, 129, 201
increased growth response of plants, 126,
199, 248
measurement of effectiveness, 125
N em agon, 206, 305
organic matter, effect, 197, 199
preparation of soil, 198-99
prior to placing containers on it, 41
selecting one to use, 1, 208-9
soil moisture, effect, 199
soil porosity, related to fumigation, 89, 142
soil temperature, effect, 148, 199
time required, 201-5
toxic residue in soil, see Chemical residue
in soil after treatment
treatment of soil in field, 18, 197, 201, 205,
206, 208-9
use near living plants, 124, 125, 200
V-C 13, 206, 305
weed control, 126, 197, 198, 200, 200-3, 204,
208, 248
when best used, 18, 197, 201, 208-9
See also Chloropicrin; DD; Ethylene dibro-
mide; Formaldehyde; Methyl bromide;
Terraclor; and Vapam
Chemicals, sources, 304—6
Chenopodium, 139
Chestnut, 46
Chickwced, spotted wilt, 235
China aster, 111, 215; Botrytis gray mold, 49-
50; chemical seed treatment, 230, 232; Fu-
sarium wilt, 5, 46-47, 49, 135, 218, 230, 232,
257-58, 260; Phomopsis canker, 233; Khizoc-
tonia on, 43, 49-50, 260; spotted wilt, 235;
Stemphylium leaf spot, 233
Chinese evergreen (Aglaonema), 226
Chloranil (Spergon), 230
Chloride in water, 64
Chloro-bromo-propene (CHI* 55), 199
Chlorophyll, 29«, 299
Chloropicrin, 200-1, 205, 206, 208, 248, 272-73
application, 16, 1H, 121,200-1,208-9
comparison with methyl bromide, 121, 198;
with steam, 121
cost, 1H, 121, 137. 197-98
effectiveness, determination, 121; in crop re
fuse, 12 1, 200; in soil. Mi, IS, 12 1
not recommended for stacked flats, 198, 201
sorption by soil, 200
sources, 304
temperatures for use, 124, 201
toxicity to crops, 124
treatment, of benches and beds, 18, 201; of
bulk soil, 18,201
used for chrysanthemums and carnations,
201, 208
used near living plants, 200
Chlorosis, of gardenia, control, 8, 107, 268;
iron, 13, 107, 113; result of biuret, 79;
result of root-infecting fungi, 15; result of
salinity, 8, 55
Choisya, water-mold root rot, 36, 37, 220
Chrysanthemum, 31, 32, 42, 203, 208, 219, 263,
268
Ascochyta ray blight, 233
aspermy virus on, 221
bacterial fasciation, 220, 233
bacterial stem rot, 35
chemical treatment of plants, 20, 232
crown gall, 220, 258
culturing technique, 20, 31, 221-22
cutting rots, 35
foliar nematode on, 20, 232
Septoria leaf spot, 233
Verticillium wilt, 7, 18, 31, 49, 201, 203, 219
virus stunt, 7, 51, 140
viruses, 232
Cineraria, 111
Citrullus (watermelon), 259
Citrus, psorosis, 232
Clarkia, 13, 111
Clay, 94, 97, 98-99, 100, 109, 142, 144, 161, 197,
199, 264, 267-68, 276
determination in fine sand, 103-4
disadvantages of, in plant culture, 12, 97;
aeration impaired, 98-99, 143; cracks
when dry, breaking roots, 268; drainage
reduced, 65-67; leaching of soluble salts
impeded, 65-67; mixing difficult, 98;
movement of fumigants and steam im-
peded, 89; shrinks from pots, 267; toxic
after steaming, 93, 96; variable chemicallv
and physically, 97, 99
effect on permeability of sand, 143
tolerances in fine sand, 103
Clay containers, hot- water treatment, 19, 53,
171-73, 211-12; salt accumulation on, 9, 53
Clods, see Lumps of soil
Clorox (sodium- hypochlorite), 216, 221, 226,
305
Clover, Persian, root-knot nematode on, 259
Coal, fuel for boilers, 161-65, 176, 191
"Cold corners" in soil steaming, 128, 134, 140;
eliminating, 128, 134, 169, 177
Colcus, foliar nematode on, 220
Collapse of plant, from damping-off, 35-36, I I,
10; from root rot, 36-37, 15; from salinity
injury, 55, 59-60
[310]
Colonization, controlled, see Controlled colo-
nization
Comb method for soil steaming (type 21), 183
Combined bin and potting bench, for soil
steaming (type 3), 132, 148, 164, 166, 168-69,
273, 278, 280-81
Competition escape in microorganisms, aerial
growth by Rhizoctonia, 251-52; in soil
microorganisms, 259; in vascular parasites,
21, 238
Competition in nursery business, means of
reducing, 32
Competitive retardant microorganisms, 21, 24,
238-40, 242, 300
Components of U. C.-type soil mixes, see In-
gredients for U. C.-type soil mixes
Compost, 91, 93, 97, 98, 99, 100; cost, 85, 100;
source of salinity, 30, 53; source of toxicity,
95; source of variability, 10
Composting, avoided by U. C.-type mixes, 89-
90, 93, 270; disadvantages, 89-90, 100; odors
and flies, 12, 90, 271; reasons for, 93-94, 109,
243; salinity problem, 90; scarcity of mate-
rials, 90; shrinkage, 89-90; source of varia-
bility, 10, 90; weed control in, 126
Computation methods, for soil particle sizes,
103-4; for steam data, 132-33, 135-37, 159-
60, 298-99
Concrete, particle sizes in, 99
Concrete mixers for soil mixing, 25, 84, 187,
265, 272-73, 276-79
Condensation, relation to steam/air ratio, 146-
51
Condensation zone in soil steaming, 128, 146,
149, 150, 152; relation to efficiency of steam-
ing, 149-52; relation to steam/air ratio, 146-
51; width of, 150, 152
Condensing capacity of soil, 149-52, 154-55
Conductance, electrical, as measure of salinity,
60-61; method of measuring, 9, 14, 60-63,
84, 299, 300, 303; of soil, 9, 61; of U. C.-type
mixes, 65, 70, 266; of water, 9, 14, 63
Conduction of heat, 149, 177; definition, 141,
299; effect of soil moisture on, 141-45; fac-
tors affecting, in soil, 141-42; importance
in soil heating, 150, 154-55; relation to
porosity, 141-42; relative importance for
heat and steam, 142; through metal con-
tainer, 142
Constant water level culture, relation to sa-
linity, 63
Container culture, advantages, 91, 234-35;
earliest example, 91-93
Containers
metal or plastic, 53, 211-12
relation to spread of pathogens, 5, 39-40,
210,217
treatment of (Section 12), 210-16; also 1, 11,
19, 48, 111, 123; required when soil treated
separately, 19, 22-23, 48, 125-27, 210, 273,
279; unnecessary for new containers, 127;
with blow torch, 19, 211; with copper
naphthenate, 19,41,212,213-16,301; with
formaldehyde, 19, 212-13; with heat, 1,
19, 211, 212; with hot water, 19, 211-12;
with methyl bromide, 19, 212; with steam,
19,40, 133, 134,211-12
Contamination problem, see Recontamination
problem
Continuous-batch steaming equipment, 16,
166, 169, 171, 174, 176
Continuous knife injector for steaming soil in
flats (type 27), 148, 165, 166, 185-86
Control of disease, 6, 48-49; benefits of, 7, 49-
51; multiple controls often needed in, 4, 219;
must mesh with nursery practices, 4, 7;
progress in, 3-4, 34-35; see also Chemical
treatment of soil; Containers, treatment of:
Dry source of heat; Hot-water treatment of
soil; Pathogen-free planting stock; Sanitary
practices; and Steam treatment of soil
Controlled colonization, 27, 250-54, 300; effect
of pH on, 251; possible future program, 24,
27, 254; relation to U. C.-type soil mixes
24, 35, 252-54; to control nitrogen nutri-
tion, 13, 25, 113-15, 116, 253-54; to retard
pathogens, 4, 20, 24-25, 35, 250-53, 254
Convection of heat, 149; definition, 141, 148;
importance in soil heating, 143, 150, 154-55;
relation to pore size, 143; relation to poros-
ity, 143; soil factors affecting, 142, 143-44
Conveyers, 26, 168, 272-73, 278-80, 282
Cooling soil after steaming, 16, 134
Copper, 95; essential to plants, 89, 107
Copper naphthenate, 19, 41, 213-16; sources,
304
Cordyline, salinity injury, 8, 9
Coreopsis, 215
Cork, heat conductivity, 299
Corn, 240-41
Corrosive sublimate, see Mercuric chloride
Cotton, 205; Fusarium wilt, 261; Rhizoctonia
on, 205, 257; Thielaviopsis on, 258
Cottonseed meal, 13, 14, 76, 105, 115-19, 121
Cottony rot, see Sclerotinia cottony rot
Covers, fitting to glasshouse benches, 180, 275;
for chemical treatment of soil, 201-3, 208,
302; for soil in steaming, 170, 178-80, 303
Cowpea, 95
Crop-antagonistic microorganisms, 22, 238-40
Crown gall, 34, 218, 220, 239; variability in
pathogenicity of bacteria, 258
Cultural practices, and disease control must
mesh, 7; evaluated only on healthv plants,
51
Culture-solution growing of plants, 87
Cultured-cutting technique, 20, 221-22, 236
Cuprinol (copper naphthenate), 19, 41, 213-16,
304
Cutting rot, 4, 35, 37, 38; see also Damping-off
Cuttings, rooted, 28, 79-80, 119, 217; soil mixes
for, 71, 72, 73, 75
[311]
Cyanamide, 244
Cyclamen, Thielaviopsis on, 258
Cymbidium, 12; salinity injury to, 8, 60; U. C-
tvpe soil mixes for, 268-69
Dagger nematode (Xiphinema), 229
Dahlia, spotted wilt of, 221, 235
Damping-off of seedlings (Section 3), 34-51;
also 4-6, 198, 202, 206
aggravated by salinity, 5, 7, 9, 33, 42, 49-50,
55, 266
causes, 4-5, 33, 37
control, 48-49; see also Control of disease
effect of carbohydrate status of host on, 5,
42-43; of depth of planting on, 5, 43; of
nitrogen status of host on, 5, 42-43; of
controlled colonization on, 24-25, 250-54;
of seed vitality on, 5, 43; of soil moisture
on, 5, 33, 36; of soil temperature on, 5, 6,
43; of watering on, 43
factors in, 5, 42-43
infection sites, 35
losses produced, 37
not restricted to seedlings, 6, 23, 36-37, 43-
44,45
recontamination problem, see Recontamina-
nation problem
relation to mechanization, 26-27, 32-33
severity related to host susceptibility, 5, 42;
to inoculum potential, 5, 42, 260; to soil
treatment, 22, 248-50; to pathogen viru-
lence, 5, 6, 260
types, 4, 35-38, 43, 249, 257
Day length, relation to plant distribution, 86
DD mixture, application, 18, 206, 209; effec-
tiveness as nematocide, 206; sources, 304
Dealers of equipment and materials, 304, 306
Decomposition of organic matter, desirable
before use, 100-1; effect of microorganisms
on, 89, 95, 237, 240-44; effect of soil oxygen
on, 240, 244; effect of soil temperature on,
240, 244; see also Organic matter
Deionized water, for leaching soil, 15, 63-64;
for watering plants, 15, 57, 63-64; not free
of boron, 64
Delphinium, 111, 263; aster yellows, 235; bac-
teria] leaf spot (black spot), 46, 47; bacterial
stem rot, 218; .sec also Larkspur
Demcton (Systox), against foliar nematode,
232; sources, 304
I) ninific ation process, 245
Deposit on leaves, salinity injury, 9, 15, 53-54,
64
Dew point . definition, 146
Di an thus, see Carnation
Dial hei m\ for soil treatment, 190
Dieffenbachia, bacterial leaf spot, 220; bac-
terial soft rot, 35, 220, 226; germinating
cane, 227; hardening for heal treatment,
223-24; heal treatmenl of cane, 220-27; pre
paring cane foi treatment, 224; Rhizoctonia
on, 220, 257; U. C. system for, 267; water-
mold stem rot, 35, 220, 226
Dieldrin, used against fungus flies, 227;
sources, 304
"Difficult" crops, 32
Diffusion of gases through soil, 89, 143, 146-
49; relation to porosity, 143, 148-49; rela-
tion to temperature, 143-44
Direct-tvpe soil heater (type 15), 165, 166, 177,
179, 195
Disease (Section 3), 34-51; also frontispiece,
11, 300; apparent vs. true cause, 33; develop-
ment of concept of, 3-4, 34-35, 138; elimi-
nation, benefits from, 7, 49-51; factors in,
5, 22, 33, 49-51, 256; importance in propaga-
tive material, 29; importance to grower, 4,
29, 49-51, 219; relation to other grower
problems, 4, 7; restricts growth potentiali-
ties of crop, 7, 49
Dish gardens, fertilizer and soil mixes for, 81,
84
Distilled water, sources, 304
Distribution system for steam, 132, 136, 195-
96; aluminium irrigation pipe, 129, 191, 195;
diameter of pipe, 191, 194, 195; efficiency,
299; heat loss in, 194; water in steam lines,
133, 152, 178, 196
Dithane D-14 (Nabam), 19, 207,209, 304
Ditylenchus, see Stem and bulb nematode
Dolomite lime, 70-75, 101, 106
Don't fight 'em, eliminate 'em, 4, 7, 23
Downy mildew of snapdragon, 46, 47
Drainage of soil, 11, 183; effect of soil condi-
tioner on, 65-67; improved by tiling, 183;
in relation to aeration, 60, 99; in relation to
salinity, 15, 53-54, 57, 64; restriction by
container boundary, 64, 87
Dreft, 230
Drenches, fungicidal and fungistatic, 207, 209;
captan (Orthocide 106), 19, 43, 207, 209,
304; combination of materials, 207; ferbam
(Fermate), 19, 207, 209, 304; nabam (Di-
thane D-14), 19, 207, 209, 304; salvage treat-
ment, 207; Semesan, 19, 207, 209, 305; Ter-
raclor (PCNB), 19, 43, 207, 209, 305; thiram
(Arasan, Iersan), 19, 43, 207, 209, 305
Dripping benches from steaming, cause, 133,
149
Drum soil Heaters, see Horizontal rotating
(hum; Oil-drum method
I)r\ fertilizers, II, 14,76,77, 79, 80
Dry source of heat for soil treatment, frontis-
piece, I, 16, 123, 162, 166, 176-77, 187, 189-91
besl with moving soil mass, 1(5, 125-26, 163
compared with steam, 125-26, 146
disadvantages, 125, 146
equipment using, 176-77
intense heal in limited area, 125
objectives, 1 1 1
temperature and time required, 15
temperature in moving soil, 127
[312]
used with dry soil, 144-46, 161, 176; with
moist soil, 145, 161, 176
Dump soil, methods for using, 84; quantity
used for bedding plants, 84
Dump truck, 168
Dura-K potassium frit, 76, 106, 304
Duratex cover for soil treatments, 178, 303
Dyes indicating liquid fertilizer injection, 76
EDB (ethylene dibromide), 18, 198, 199, 206,
209, 304
Eddy currents of steam in soil, 149
Efficiency calculations for soil steaming, 299
Eggplant, 25-26, 41, 264-65
Egypt, nurseries in, 91
Einheitserde (standardized soil), 94, 96
Electricity, power for boilers, 16, 162, 163, 164—
65, 176, 177, 184, 185, 190, 192, 195
Environment, effect on disease, 5, 29-30, 42-
43, 44, 49-50, 300; effect on plant, 5, 42-43,
86-89
Environmental tolerance of crop, 49
Equipment, fumigation of, 138
Equipment for mechanized fertilizer applica-
tion, 76, 78, 283-84
Equipment for mechanized watering, 27, 283-
84
Equipment for planting, Erdprinz planter,
282-83, 302; machine seeding, 25-26, 264,
283; pot and can fillers, 25, 26, 33, 166, 168,
272-73, 280, 302
Equipment for soil handling (Section 17),
275-82, also 25-26
bicycle-wheel cart for pots, 281-82
breaking up lumps, 98, 133, 161
can filler, 25, 26, 33, 166, 272-73, 280, 302
concrete mixer, 25, 84, 187, 265, 272-73,
276-79
conveyers, 26, 168, 272-73, 278-80, 282
enclosed storage building, 163-66, 275-76
flat filler, 25, 26, 166, 168, 272-73, 279-80
fork-lift tractor, 25, 26, 166, 171, 174, 211,
272-73, 277-79, 280-81
mobile bin and potting bench (type 3), 132,
148, 164, 166, 168-69, 273, 278, 280-81
moving belts, 26, 168, 272-73, 278-80, 282
pot filler, 25, 168, 272-73, 280, 282, 302
screen, 276-79
shredder, 98, 276
skip-load tractor, 25, 84, 168, 272-73, 276,
278-79, 280
soil treatment, see Equipment for soil heat-
ing, below
steel rollers, 25, 272-75, 277, 279, 282
wooden pallet, 22, 25, 26, 166, 171, 174, 211,
212, 272-73, 276-77, 279, 280-81
Equipment for soil heating (Section 10), 162-
96; also 1, 16
adapting batch equipment to continuous
operation, 16, 166, 169, 171, 174, 176
autoclave (type 9), 16, 17, 25, 129, 132, 134,
147, 151, 158, 162, 164, 166, 174-75, 272
baking or burning (type 17), 165, 166, 177
box, electric heating elements (type 14), 1 12,
165, 166, 176-77, 179, 195, 303; tubular
version, 177
box, electrode heating (type 15;, 165, 166,
177, 179, 195
box, induction grid (type 16), 165, 166, 177,
195
bulk units, 15, 16, 167-77, 185-91
buried perforated pipe (type 20), 16, 128,
131, 132, 138, 148, 150, 152, 156, 165, 166,
178, 180-83, 184, 194
buried tile (type 22), 16, 131, 132, 118, 156,
165, 166, 178, 181, 183, 185
combined bin, potting bench (type 3), 132,
1 18, 164, 166, 168-69, 273, 278, 280-81
containers, treated in, 162, 164-65
continuous knife injector for flats (type 27),
148, 165, 166, 185-86
deep steaming of benches or beds, 131, 178,
180-83
efficiency levels, 132
electric hot-plate type (type 32), 165, 189-
90, 195
free-flowing vs. superheated steam, 129-30,
156-59
horizontal tank (type 13), 131, 164
horizontal type with removable hood (type
10), 131, 164, 174-76, 195,272
hot water (type 25), 16, 148, 165, 182, 184
inverted pan, electric (type 24), 148, 165,
178, 180-81, 184, 195
inverted pan, steam (type 19), 16, 131, 132,
138, 148, 165, 166, 178, 180-81, 184, 275
mobile bin (type 2), 16, 132, 148, 164, 166,
168, 193, 273, 280-81, 303
mobile units, 162, 273
movable Thomas method for ground beds
(type 18), 148, 166, 180
moving rake (type 23), 131, 148, 165, 166,
178, 182-84
multipurpose tank (type 7), 16, 131, 132,
148, 164, 166, 171-73, 176
oil-drum type (type 12), 131, 164, 176
permanent vs. mobile equipment, 163, 164-
65
rotating drum, external flame, batch (typs
35), 165, 191, 303
rotating drum, external flame, continuous
(type 31), 165, 190,273
rotating drum, internal flame (type 30),
165, 185, 187, 189-90, 194, 303
rotating drum, knife injector (tvpe 28), 14S,
165, 166, 185-87, 273
rotating screw, electric (type 33), 165, 189-
90, 195; external flame (tvpe 34), 165, 190
rotating screw, steam (tvpe 29), 16, 165, 187-
88, 272, 303
[313]
Equipment for soil heating, continued
Rudd type (type 1), 132, 148, 164, 166, 167-
68, 180
self-generating types of steamers, 174-76, 184
shallow steaming of benches or beds, 131,
178-80
sources, 302-4
spike or rake type (type 21), 135, 1 18, 150,
165, 166, 178, 181, 183
stationary units, 162, 166-77
stationary vs. moving soil mass, 16, 162-63,
166, 185
steam box, bulk and containers (removable
front) (type 4b), 16, 17, 131, 132, 148, 156,
164, 166,' 169-70, 303
steam box, bulk soil (fixed front) (type 4a),
16, 132, 148, 156, 164, 166, 167, 169-70, 176,
273, 303
steam-chemical (type 26), 148, 165, 166, 184-
85, 213
steam-generating equipment, see Steam-
generating equipment
steam plow, 182
steam vs. dry heaters, 125, 141
table for selecting suitable type, 164-65, 274
Thomas, for beds (surface) (type 18), 16, 131,
132, 148, 163, 165, 166, 171, 178-80
Thomas, for containers (type 5), 16, 131,
132, 148, 164, 166, 170-71, 179, 272
tipping steam box, Norwegian, 167
vault type (type 6), 16, 25, 131, 132, 148,
164, 166, 167, 171-72, 174, 272,277, 280-81
vertical cabinet, electric (type 11), 131, 174,
175-76
vertical cabinet, external steam (type 8),
131, 132, 148, 164, 166, 173-75, 176
vertical cabinet, self-generating (type 11),
131, 164, 174, 175-76, 195
Equipment for soil testing, 302
Equivalents, table of, 301
Eradication of pathogen, difficult in field, 197;
from tools, 19, 22, 23, 40, 48, 201, 226; in
host tissue, 20, 223; see also Chemical treat-
ment of soil; Containers, treatment; Dry
source of heat; Hot-water treatment of soil;
and Steam treatment of soil
Erdalith for wood preservation, 215, 216
Erdprinz planter for pots, 282-83, 302
Erica, see Heather
Esther Read daisy, see Chrysanthemum
Ethylene dibromide (EDB), application, 18,
206, 209; effectiveness, 198, 206; residual
toxicit) to plants, 199, 206; sources, 304
Eth) lene oxide, 216
Euphorbia (poinsettia), 29, 257, 258, 266
Evolution ol plants, 86, 91, 109
lasuat ion, bacterial, 220, 233, 258
Ferbam (Fermate), 19, 207, 209, 22!), 304
Ferns, foliar nematode on, 233; salinity injury,
7, 58-59
Fertility, of clays and composts, 99-100; of fine
sand-peat mixtures, 12, 99-100
Fertilizer burn, aggravates Botrytis diseases, 46
Fertilizer ingredients of U. C.-type soil mixes,
69-76
1,71-75,77, 78, 79,80, 81, 111
11,71-75, 79, 80, 81, 111
111,71-75,80, 111
IV, 71-75, 77, 78, 79,80, 81, 111
V, 71-75, 79, 80, 81, 111
VI, 71-75, 80, 111
cost, 71-75
mixing, 70
salinity from, 15, 53-54, 57
Fertilizers, 76-79, 87, 96
deficit, effect on plant, 88
dry, 14; application methods, 11, 14, 76-77,
79; formulas (fertilizers VII-XI), 76-77;
use, examples, 79, 80
evaluation, 51
excess, cause of chlorosis, 107
inorganic, see Ammonium and Nitrate ni-
trogen
liquid, 14; application during watering, 14,
27, 76, 78; formulas (fertilizers L-l to L
12), 76, 78; proportioned for applying,
283, 302; use, examples, 78-81
mechanized application, 78
organic, mixed in soil, 71-75, 122; on sur-
face, 13-14, 118-19, 121, 122
source of salinity, 9, 11, 15, 30, 53-54, 57,
64-65, 70
Fertilizing equipment, 204, 302
Fiberthin covers for soil treatments, 178, 303
Fillers, can, 25, 26, 38, 166, 272-73, 280, 282,
302; flat, 25, 26, 166, 168, 272-73, 277, 279-
80; pot, 25, 168, 280, 282, 302
Fine sand, see Sand, fine
Fir, Douglas, 46; bark, 65-67
Fire blight, 34, 258
Fish meal, 13,76, 115-19, 121
Fittonia, hardening for heat treatment, 223-
24; heat treatment of plants, 227-28, 229;
Rhizoctonia on, 220-21, 227-28, 267; U. C.
system for, 267; water-mold root rot, 220-
21,267
Flash-flame pasteurizer for soil (type 30), 187—
88, 190
flash steamers, 192, 302
Flat -making machine, 33, 276
Flats, 126, 127, 150, 163, 196, 197, 201, 210,
219, 250, 254; chemical treatment, 1, 19, 10,
201, 203, 201, 208, 212-16; fertilizer schedule
lor plants, 79; filler, 25, 26, 166, 168, 272-
73, 279-80; si/e, 279, 301; soil mixes for, 12,
69, 72, 75, 79, 264-65; stacking for soil treat-
ment, 131, 173, 189, 201-4, 211: steam treat-
ment, 19. 10, 133. 13 1, 162, 163, 170, 171,
173, 211; transporting, 22, 25, 26, 166, 171,
171, 21 1. 212, 272-73, 276-77. 279, 280-81
[314]
Flies from compost piles, 12, 90, 271; from
organic nitrogen, 122
Floricultnral plants, 28
Flower blights, 34
Foliage plants, 20, 29, 32; U. C. system for, 20,
29, 32, 266-67; utilize ammonium, 13
Foliar feeding, 89
Foliar nematode (Aphelenchoides), 20, 47, 220,
233; chemical treatment of plants against,
232; lethal temperatures, 139
Fork-lift tractor, 25, 26, 166, 171, 174, 211.
272-73, 277-79, 280-81
Formaldehyde. 200, 203-4, 208
dilute method for soil, 204, 208; relation to
inoculum potential, 42, 204, 260
effectiveness, 203
paraformaldehyde formation, 19, 212-13
sources, 304
steam-formaldehvde for soil treatment, 148,
184; for glasshouse cleanup, 213
toxicity to plants. 204
treatment, of containers, 19, 212-13; of floor,
18, 22, 134, 166, 199; of planting material,
20, 228, 230; of soil, drench, 41, 148, 204,
208; of tools, 19, 22, 23, 40, 213, 226
Formalin, see Formaldehyde
Fragaria (strawberry), 220
Frankincense trees, 91
Free-flowing steam for soil treatment, 15, 129,
135, 157-58, 164-65, 167-74, 178-84, 187,
191-92, 196, 300; advantages, 129; heat con-
tent, 157-58; pressure in mains, 129
Freesia, mosaic, 21, 233
Frit, potash, 76, 106
Frost, relation to plant distribution, 86
Frozen soil, cause of uneven steaming, 134
Fuchsia, foliar nematode on, 220
Fuel for steam boilers, 16
amount required for soil treatment. 135-36
butane, 16, 162. 187, 192, 194
coal, 164-65, 176, 194
cost, 136
electricity, 16, 162, 163, 164-65, 176, 177,
184, 185, 190, 192, 195
heating value, 299
kerosene, 187, 194
natural gas, 16, 135, 136, 162, 163, 164-65,
174, 176, 185, 187, 190, 191, 192, 194
oil, 16, 136, 162, 163, 164-65, 174, 176, 185,
190, 192, 194
propane, 162, 192, 195
Fumigants, see Fungicides and Xematocides
Fungi, 15, 18, 197, 198, 200, 204, 206, 221, 237-
38, 242, 254, 299; longevity, 199, 243: nema-
tode-trapping, 240; variability, 255-58; see
also Damping-off
Fungicides, 259, 299
captan (Orthocide 406), 19. 43, 207, 209, 304
Celcure, 216
chloropicrin, see Chloropicrin
copper naphthenate (Cuprinol), see Copper
naphthenate
Erdalith, 215, 216
ethylene oxide (Carboxide), 216
ferbam (Fermate;, 19, 207, 209, 228, 301
formaldehyde, see Formaldehyde
mercuric chloride, 20, 230, 232
methyl bromide, see Methyl bromide
nabam (Dithane D-14), 19, 207, 209, 30!
New Improved Ceresan, 20, 230
Puratized Agricultural Spray, 228, 305
Semesan, 19, 207, 209, 305
sodium hypochlorite (Clorox, Purex), 216,
221-22, 226, 305
sources, 304-6
Spergon (Chloranil), 230
sulfur, 246-47
Terraclor (PCNB), 19, 43, 205, 207, 208-9,
305
thiram (Arasan, Tersan), 19, 43,207, 209, 305
Yapam, 18, 204-5, 208, 305
Wolman salts, 215, 216
Fungistatic, 299
Fungus flies, control, 227; spread soft-rot bac-
teria, 227
Fusarium, 198, 220,250
basal rot, 227-28
cortical root rot, 229, 256
cortical stem rot, 256
effect of soil temperature, 260
lethal temperatures, 127, 139
longevity in soil, 261
saprophytes and parasites in soil, 238
saprophytic, 256
survival in soil, 261
variability, 256-58
vascular wilts, 139, 256-57
wilt, favored by nematodes, 261
Fusarium wilt of China aster, 5, 135, 230, 232,
257-58; conditions favoring, 47, 49, 260; in-
oculum potential, 260; life history of causal
fungus, 218; relation to Botrvtis crown rot,
49; relation to Rhizoctonia crown rot, 49;
soil temperature, 260; symptoms, 46-47
Galvanized nails, corrosion bv copper naph-
thenate, 213
Gardenia, 35, 69, 268; chlorosis, 8, 107, 268;
salinity injury, 8, 55, 59-60; U. C. system
for, 268
Gas, natural, fuel for boilers. 16, 135. 136,
162, 163, 164-65, 174, 176. 185. 187. 190. 191.
192, 194
Gases, viscosity related to temperature. 143
Geranium. 29, 32, 35, 215-16; bacterial leaf
spot and stem rot of. 21. 35, 261: cultured-
cutting technique with, 20, 221; mosaic of.
234
Gerbera, heat treatment of plants. 227; root-
knot nematode, 227
German peat, see Peat, sphagnum
[315]
Germination
effect of pelleting on, 25, 283; of salinity on,
9, 42, 55
in mechanization, 26-27, 264
rate, seed, 82; effect of soil toxicity on, 94
Gladiolus, 223, 263; effect of soil temperature
on heat tolerance of cormels, 224; heat treat-
ment of cormels, 224; presoaking cormels
before heat treatment, 224; Rhizoctonia on,
257; yellows disease, 139
Glossary of terms used, 298-301
Glycine (soybean), 257
Gossypium (cotton), 205, 257, 258, 261
Graft failure, Thielaviopsis, 258
Gravel, 97, 98, 99, 100, 103-4
Gray mold (Botrytis), 5, 9, 46-47, 49-50, 139
Grower experience with U. C. system (Section
16), 263-70; also 1; bed flower crops, 208;
bedding plants, 264-65; bench flower crops,
268; can -grown woody stock, 267; cymbi-
diums, 268-69; foliage plants, 266-67; land-
scape application, 269-70; pot plants, 266-
67; vegetable transplants, 265-66
Grower "secrets," 49
Growing-on, soil mixes for, 71, 73, 74
Growth regulators, 51
Gypsum, source of calcium, 71-72, 101, 106;
used to reduce soil toxicity, 10, 96, 109; see
also Calcium sulfate
Hardpan in soil, and salinity, 57
Harrow method of soil steaming, see Spike
method
Harrow-type electrode heater (type 15), 165,
166, 177, 179, 195
Haworthia, heat treatment of plants, 139, 227;
Pythium root rot, 139, 227
Heat, definition, 141; differentiated from
steam, 142
Heat capacity, definition, 141, 299, 301
Heat requirement of soil, 299; of water, 299
Heat sterilization, development of, 138; of
containers, 1, 19,211,212
Heat-tolerant plant parts for treatment, 223-
24
Heat transmission
compared with steam movement, 1 11-45
conduction, 141-42, 111, 150
convection, 141, 142, 143-44, 148, 150, 151-55
radiation, 141, 142, 144, 150
rate, in dry soil, 144-45; in moist soil, 144-45
) elation to compaction, 130, 134, 112; to or-
ganic mattei content, 112; to particle size,
I 12; to soil porosity, I 11-12; to soil mois
line-. 111 1")
Stead) and misleads states, 145-46, 150
through pine logs, 151-52
I leal treatment
of planting material, 138, 236; against
microdrganisms, 139, 223-31; againsl
viruses, 221; See also Hot-water treatment
of planting material
of soil (Sections 8, 9), 123-61; also 11, 210; see
also Dry source of heat for soil treatment;
Hot-water treatment of soil; and Steam
treatment of soil
Heather (Erica), chlorosis, 107; cutting rot,
45; Phvtophthora root rot, 7, 45, 49, 218-19,
220, 258; Rhizoctonia stem rot, 220
Heating of soil, effect on organic nitrogen
breakdown, 13, 53, 105, 112, 115-19, 120
Hedera (ivy), 220-21, 267
Helichotylenchus (spiral nematode), 229
Helminthosporium cactorum, 38
Herbaceous ornamentals, 29
Heterodera, see Potato root nematode and
Root-knot nematode
High vs. low pressure steam for soil treatment,
191-92
Hippeastrum (amaryllis), 58
"Hoddesdon pipe" for soil steaming, 180;
winch-drawn, 182
Home-yard planting, fertilizer schedule, 80-
81; soil mixes, 81, 84; steaming soil, 135, 193
Hoof and horn meal, 13, 14, 53, 70-75, 76, 77,
79, 91, 105, 106, 110, 111, 112, 113, 115-19,
121,242,243
Horizontal rotating-drum soil heaters, exter-
nal flame, batch type (type 35), 165, 191, 303;
external flame, continuous type (type 31),
165, 190, 273; internal flame (type 30), 165,
185, 187, 189-90, 194, 273, 303; knife-injec-
tor type (type 28), 148, 165, 166, 185-87, 273
Horizontal rotating-screw soil heaters, electric
(type 33), 165, 189-90, 195; external flame
(type 34), 165, 190; steam (type 29), 16, 165,
187-88, 272, 303
Horizontal tank-type soil steamer (type 13),
131, 164, 176
Horizontal-type steamer, removable hood
(type 10), 131, 164, 174-76, 195, 272
Hormone solutions, relation to spread of
pathogens, 5, 22, 38
Horsepower rating of boiler vs. pounds of
steam, 159-60
Hose nozzle and spread of pathogens, 5, 23, 24,
38-40
Host, 299, 300
Host range of pathogens, 6, 256-59; variability
in. 256-59
Hot-plate method of soil heating (type 32),
165, 189-90, 195
Hot-water treatment of containers, methods,
19; salt removal, 19, 211-12
Hot-water treatment of planting material. 20,
Hi I 65,223-30,236
application to specific crops, 226-30
breaking dormanc s of stock. 227. 229, 230
conditioning the material, 20, 223-24
containers lor material. 225
cooling the material, 225-26
[ 316 ]
drying the material, 226
equipment, 302
eradication of pathogens, 20, 223
methods, 223-26
multipurpose tank, 171-73, 224
not protective against reinfection, 223
preparing the material, 20, 224
presoaking the material, 224
selecting material to treat, 223
storing the material, 226
temperature-time relation, 20, 139, 225
treatment tanks, 224-25
value, 223
Hot-water treatment of soil, 123; compared
with steam, 126, 146-48, 152, 156-57, 184;
disadvantages, 126, 146; equipment for
heating by steam (type 25), 16, 148, 165,
182, 184; excessive water, 126, 184; heat con-
tent of hot water, 146, 156-57; heat transfer
involved, 146, 156-57; salt removal, 126, 146,
184; use on propagating sand, 126, 146, 184
Humidity, atmospheric, 146-47; effect on dis-
eases, 29-30, 42-43; on salinity injury, 11,
15
Humus, 99
Hutchings method for soil heating (type 32),
165, 189-90, 195
Hybrid seed, 32
Hyacinth, stem and bulb nematode on, 258
Hydrangea, blue vs. pink, 76
Hypericum, 139
Hypnum peat moss, 69, 104
Iceland poppy, 111, 215
Immersion-type soil heater (type 14), 142, 165,
166, 176-77, 179, 195, 303
Increase block, 222, 235-36
Increased growth response from soil treat-
ment, 126, 199, 248
Incubation period of disease, 232, 234
Indirect-type soil heater (type 14), 142, 165,
166, 176-77, 179, 195, 303
Induction-grid type soil heater (type 16), 165,
166, 177, 195
Infected seed or stock, 43, 44, 260; increase of
inoculum potential, 260; means of selecting
virulent strains, 6, 260
Infection, 299; by Rhizoctonia, 38
Infest, definition, 299
Infrared lights for soil heat treatment, 190
Ingredients for U. C.-type mixes, 12-13, 69-
76, 96-107
aeration, 97, 98-99
availability, 12, 97, 98, 103
characteristics, 101-7
chemical, 69-76, 97, 98, 101, 105-7; see also
Fertilizer ingredients
cost, 97, 100
criteria for selection, 96-107
ease of mixing, 83-84, 97, 98, 105, 133, 276-
79
fertility, 97, 99-100, 105-7
moisture retention, 12, 69, 87, 97, 100, 270
physical, 69, 101-5; see also Peat, sphagnum;
Redwood; Rice hulls; and Sand, fine
proportions, 69-76
resistant to leaching of nutrients, 12, 97, 99
selection, 96-107
shrinkage, 12, 80, 85, 89-90, 97, 100-1, 241
soil used, low in organic matter, 103
sources, 85, 97-98, 101-3, 275
stability to steaming or fumigation, 9-10,
11, 12, 15, 90, 93, 96, 97-98, 124, 129, 140,
199,270
uniformity, 12, 97, 98
weight, 12,69, 80,97, 100
Injector, for applying fertilizers, 283, 302; for
applying soil fumigants, 200, 201, 206, 302
Inoculation of soil, with ammonifying micro-
organisms, 13, 113-15; with antagonistic
microorganisms, 4, 20, 24-25, 35, 250-54;
with nitrifying bacteria, 13, 25, 113-15, 116,
120, 253-54
Inoculum potential, 5, 42, 204, 260, 300
Insect screens on seedbeds, 235
Insecticides, 18, 20, 206, 227, 232, 304, 305
Insects and mites, 15, 18, 21, 138, 197, 198, 200,
204, 206, 248, 275; lethal temperatures, 127,
139
Inserts for flats, 25, 31, 127
Introduction of new disease, importance, 20,
218; see also Spread of microorganisms
Inverted pan for soil steaming (type 19), 16,
131, 132, 138, 148, 165, 166, 178, 180-81, 184,
275; electric type (type 24), 148, 165, 178,
180-81, 184, 195
Ipomoea (morning-glory and sweet potato',,
221,257
Iris, 139, 260
Iron, 95; availability affected by microorgan-
isms, 237, 247; chelate for chlorosis, 107, 268;
chlorosis, 13, 107, 113; essential to plants,
89, 107
Isolation house, 21, 23, 24, 234-35, 261
Ivy, bacterial leaf spot, 221; Rhizoctonia on,
220-21; U. C. system for, 267; water-mold
root rots, 220-21
John Innes composts, 10, 86, 91, 93; contribu-
tion to nursery soils, 10, 91, 93, 110; disad-
vantages, 93, 96; sold on market, 94
John Innes high-rate soil steamer (type 1),
167-68
Kentia palms, 284
Kerosene, fuel for boilers, 187, 194
Kilowatt-hours, 159, 300
Klamath-weed seed, heat resistant, 139
Krillium, effect on leachability of soil, 15,
65-67
L 317 J
Labor, cost rising, 32, 96, 196, 271; reduced by
U. C.-type soil mix, 10, 84, 89-90, 100, 270
Lactuca (lettuce), 95, 112
Lamb's quarter seed, heat resistant, 139
Landscape use of U. C. system, 269-70; soil
fumigation in field plantings, 269-70
Land value rising, effect on nurseries, 31
Larkspur, 215
Lathyrus (sweet pea), 230
Leachability of U. C.-tvpe soil mixes, 65-67,
99
Leaching
losses of soil nutrients, 65-67, 99, 105-7
to reduce salinity, 9, 11, 14-15, 183; effec-
tiveness related to water salinity, 9, 14,
63; relative leachability of various soil
mixes, 15, 65-67; with nutrient solution,
65
to reduce toxicity, 10, 95, 96
Leaf burn, from ammonium, 13, 111, 113;
from biuret, 79; from salinity, 8-9, 42, 55-
56, 58
Leaflet on U. C.-type soil mixes, 68
Leaf mold, 86, 97, 98, 99, 115-19, 242, 262, 267,
268
aeration when decomposed, 99
cost, 85, 100
scarce in California, 12, 90, 98, 100
shrinkage, 85, 90
source of salinity, 9, 15, 30, 53-54, 90, 264;
of toxicity, 95, 108; of variability, 10, 89,
93
Leaf spots, 34
Legumes, 77, 78, 245
Lesion nematodes (Pratylenchus), 47, 227, 229;
lethal temperatures, 139
Lettuce, ammonia toxicity, 112; manganese
toxicity, 95
Light on plant, 29, 51, 259; relation to damp-
ing-off, 5, 43; relation to plant distribution,
86
Light soil mix, 93; see also U. C.-type soil
mixes
Lignin, 254
Lily (Lilium), 86; Fusarium basal rot, 227,
229; root development in U. C.-type soil
mix, 83 (fig. 61); treatment of bulbs against
nematodes and Rhizoctonia, 227-28, 229
Lima bean, Rhizoctonia on, 257
Lime, 70. 91, 101, 115, 120; calcium carbonate,
70, 72-75, 91, 101, 106; dolomite, 70-75,
101, 100; ovstei shell, 106
Liners, soil mixes for, 71, 72, 73, 80
Lining-out slock, 29
Liquidanibar , chlorosis, 107
Liquid fertilizers, 14, 27, 76, 78-79, 106; pro
portioners for applying, 283, 302
Little-leaf of peach, 248
"Living uilh" a disease, 7, 49
Loam, 15, 65-67, 91, 97, 98, 99, 100, 1 12, 1 13,
I 11, I") I 55
Lobelia, 111,215
Lobularia (sweet alyssum), 13, 111, 112, 113,
264
Loganberry, crown gall, 258
Longevity of organisms in soil, 261
Long pipe for soil steaming, 180, 184; winch-
drawn, 182, 184
Lotus strigosus seed, heat resistant, 139
Lumps of soil, equipment for breaking up,
98, 133, 161; not formed by fine sand, 98,
133, 161, 276; relation to chemical treat-
ments, 199; relation to steaming, 15, 127,
133, 134, 140, 149, 160-61, 190
Lycopersicon, see Tomato
Machinery, disinfestation, 201, 212
Magnesium, 64, 95, 99, 109, 110; availability
affected by microorganisms, 237, 247; es-
sential to plants, 89, 106; from dolomite
lime, 13, 70
Magnesium bicarbonate, 63
Magnesium carbonate, 106
Magnesium sulfate, 94, 177
Maidenhair fern, 215
Maintenance of pathogen-free planting stock,
21, 226, 234-36; by selecting growing area,
21, 233; of chrysanthemums, 31
Majestic daisy, see Chrysanthemum
Malathion, against fungus flies, 227; sources,
304
Mains (apple), 258; see also Fire blight
Malva (buttonweed), 139, 203, 235
Manetti, see Rose
Manganese, availability affected by micro-
organisms, 247-48; essential to plants, 89,
106-7; role in soil toxicity, 9, 95, 98
Manure, 97, 98, 115-19, 198, 241-42, 262, 264,
265, 267, 268, 271
aeration, when decomposed, 99
competition, 12, 90
cost, 85, 100
package trade, 90
poor source of nutrients, 99, 100; of organic
matter, 89, 100
shrinkage, 85, 89-90, 100, 241
source, of salinity, 9, 30, 53-54, 90, 116; of
toxicity, 95, 108; of variability, 10, 89, 93
Maple leaves, 100
Maranta, salinity injury, 8-9
Marguerite, see Chrysanthemum
Marigold, see Calendula and Tagetes
Market, distance from, 31-32; expanding in
California, 31-32; lor bedding plants, 30-31
Materials, sources, 302-6
Matthiola, see Stock
Meadow nematode (Pratylenchus), 17, 139,
227, 229
Measures, table of, 301
Mechanical applicators of fumigants, 201.
20 1 -5, 200
[318]
Mechanization in growing (Section 17), 271-
84; also frontispiece, l', 25-27, 32, 33, 266
adaptability of U. C. system to, 25, 90, 94,
270,271
adoption when moving, 31
advantages of sloping land for, 32, 274
applied to new nursery, 274-75; to old
nursery, 274
bicycle-wheel cart, 281-82
disease control required, 26-27, 32-33
fertilizing, 78, 204, 283-84, 302
filling containers, 25, 26, 33, 166, 168, 272-
73,^ 279-80, 282, 302
flat-making machine, 33, 276
flow diagrams, 1, 272-73
germination in covered flats, 26-27, 264
glasshouse arrangement and design, 275
laird slope in mechanization, 32, 274
machine planting, 25-27, 264, 283, 302
mixing and screening soils, 25, 83-84, 97,
98, 187, 265, 272-73, 276-79
mobile bin and potting bench (type 3), 132,
148, 164, 166, 168-69, 273, 278, 280-81
paving the yard, 275
planning layout, 31, 274-84
planting, 25-27, 264, 283, 302
preparing soil mixes, 83-84, 105, 133, 276
processing and stockpiling materials, 275-77
requirements to make possible, 26-27, 32-33
seeding in place, 25-26, 264, 283, 302
segregation of operations, 21, 163, 166, 276
storage of components, 275-76; of soil mixes,
13, 25, 71-75, 276
transplanting, 25, 81, 264, 282-83
transporting containers, 281-82; soil, 25,
280, 282
watering operation, 27, 283-84
See also Chemical treatment of soil; Con-
tainers, treatment of; Dry source of heat
for soil treatment; Hot-water treatment
of soil; and Steam treatment of soil
Medicago, see Bur clover and Alfalfa
Meloidogyne, see Root-knot nematode
Mercuric chloride, treatment of planting
stock, 20, 230, 232
Methyl bromide, 143, 200, 201-3, 206, 208-9,
264, 267, 269, 272-73
application, 16, 18, 124, 198, 201-2, 204
cost, 18, 124, 137, 197-98
effectiveness, determination of, 124; in crop
refuse, 124, 203; in soil, 16, 124
ineffective against Verticillium, 16, 18, 22,
124, 203
residual toxicity to plants, 16, 124, 199
sources, 304
steam-methyl bromide for soil treatment,
185
temperatures for use, 124, 201-2
toxicity to crops, 10, 16, 17, 18, 124, 199, 208
treatment, of containers, 19, 212; of farm
machinery, 201, 212; of soil in stacked
containers, 18, 201-2, 272
use in "pinto tag" certification, 48, 129, 201
Micronutrients, 106-7; supply in U. C.-type
mixes, 12, 89, 101, 106-7, 109, 110
Microorganisms, soil (Section 14), 237-54
abundance, 237-38
antagonistic, 4, 20, 21, 24-25, 35, 250-54
balanced population, 21, 25, 238-40, 250-54
beneficial, 238-40
buffering capacity, 299
carbon cycle, 246-47
cause of disease, 3, 4, 33-35, 138
competition, 21, 24, 238-40, 242, 300
concentration in rhizosphere, 240-41; in
surface layer, 120, 238, 240
controlled colonization, see Controlled colo-
nization
crop-antagonistic, 22, 238-40
decomposition of organic matter, 89, 95,
115-19,237,240-44
dependence on green plants, 241
depth in soil, 6, 120, 238, 240
distribution, 240
dynamic equilibrium, 21, 25, 238-40, 250-
54
effect of fungicide dosage on, 249-50; of
organic matter on, 25, 238, 240, 242-44;
of oxygen on, 121, 240, 244, 298; of soil
moisture on, 21, 25, 49-50, 240; of pH on,
120-21, 245-48; of soil treatment on, 19,
113-15, 115-19, 120, 204, 205, 248-50; of
soil temperature on, 21, 25, 240, 244
fermentation, 138
harmful, 238-40
having the same name, 23, 255-62
included in this manual, 34
injurious to plants, 238-40
inoculum potential, 5, 42, 204, 260, 300
nitrogen cycle, 245-46
nutrient requirements, 242-44
release nutrients in soil, 89, 237, 244-48
retardants to pathogens, 4, 20, 21, 24-25, 35,
250-54
spread, see Spread of microorganisms
survival in soil, 21, 238, 243, 261
types 1 and 2 in nitrogen conversion, 245,
254
variability, 255-59
Minerals supplied by soil, 10, 89, 138
Mix, soil, see Soil mixes and U. C.-type soil
mixes
Mixed infections, 261
Mixes, fertilizer, see Fertilizer mixes and Fer-
tilizers
Mixing, U. C.-type soil, 83-84, 97, 98, 105. 133,
276-79; uneven, effect on steaming, 134
Mobile bin for soil steaming (type 2), 16, 132,
148, 164, 166, 168, 193, 273, 280-81, 303
[319]
Moisture
soil, 29, 87-88, 120, 125, 300; deficiency, ac-
cumulative effect of, 87-88; relation to
damping-off, 5, 49-50; relation to salin-
ity measurement, 61; see also Soil, mois-
ture
supplied by soil, 87
Molybdenum required by plants, 89, 107
Mono-ammonium phospbate, 14, 78
Monocalcium pbosphate, 70, 106
Morning-glory, Rhizoctonia on, 257 (fig. 124)
Mosaic, anemone, 21, 233; carnation, 234; cel-
ery, 265; freesia, 21, 233; geranium, 234; po-
tato, 221; ranunculus, 21, 233; rose, 7, 21,
51, 232, 236; stock, 235; tobacco, 140
Mosses, 211
Mother block (nucleus block) propagation,
21, 31, 222, 235-36; maintaining horticul-
tural quality, 235
Movable Thomas method for ground beds
(type 18), 180
Moving rake method of soil steaming (type
23), 131, 148, 165, 166, 178, 182-84
Multiplicity of nursery soil mixes, disadvan-
tages, 89-90, 93, 264-65
Multipurpose tank (type 7), 16, 131, 132, 148,
164, 166, 171-73, 176; for hot-water treat-
ment of stock, 171-73; for removing salts
from containers, 171-73; for soil and con-
tainer treatment, 164, 166, 171-73
Muriate of potash (potassium chloride), 14,
76, 77, 78, 106, 305
Mushroom growers, 90
Mustard, host of stock mosaic, 235; seed heat
resistant, 139
Mycelium, 38, 39, 44-45, 300
Myrothecium as a retardant, 25; effect of ad-
ding cellulose to soil on, 251, 253; inhibits
Rhizoctonia, 25, 251, 253; may stunt plants,
251, 253
Xabarn (Dithane D-14), 19, 207, 209; sources,
304
Narcissus, stem and bulb nematode on, 258
Nasturtium, 215; presoaking seed before heat
treatment, 224; spotted wilt, 235
Necrosis of plant, caused by soil toxicity, 9,
91-95; bv damping-off, 35-37, 44-45; by sa-
linity, 7-9, 55-56, 58-60
Nemagon, 206, 305
Nematorides, 18, 21, 198, 206, 208; chloropk-
rin, 18, 208; I)D mixture, 18, 206, 209, 304;
ethylene dibromide (EDB), 18, 198, 199,
206, 209, 804; may increase losses from
fungi, 261; methyl bromide, 18, 208-9; Ne-
magon, 206, 305; sodium selenate (P- 10).
232, 305; Vapam, 18, 204-5, 208; V-C 13,
206, 805
Nematodes, 55, 200, 206, 238, 800
control, 15, L8, 107, I OH, 202-3, 203-5
daggei (Xiphim ma), 229
foliar (Aphelenchoides), 20, 47, 139, 220,
232-33
fungi which trap, 240
longevity in soil, 261
meadow (Pratylenchns), 47, 139, 227, 229
potato root nematode (Heterodera), 139
root knot (Meloidogyne), see Root-knot ne-
matode
root lesion (Pratylenchns), 47, 139, 227, 229
spiral (Heiichotylenchns), 229
stem and bulb (Ditylenchus), 47, 139, 227,
258
sting (Belonolaiynus), 261
survival in soil, 261
symptoms, 47
variability, 258-59
Nemesia, 215
Nephthytis, hardening for heat treatment,
223-24; Rhizoctonia on, 220-21; U. C. sys-
tem for, 267; water-mold root rot, 220-21
Nerium (oleander), 220
New Improved Ceresan, treatment of planting
stock, 20, 230
New York soil heater (type 14), 142, 165, 166,
176-77, 179, 195, 303
Nicotiana (tobacco) 82, 140, 214, 215, 248, 258,
261
Nitrate nitrogen, 13, 95, 105, 109, 111, 115,
116-19, 122, 243, 245, 253-54; leachability
from soil, 109; when to use as fertilizer, 14,
105
Nitrifiers, see Nitrifying bacteria
Nitrifying activity in soil
effect of soil depth on, 114-15, 238, 240; of
low organic nitrogen on, 116-18; of pH
on, 13, 120-21, 245-46; of temperature on,
13, 115-19, 121, 245-46
elimination by steaming, 13, 95, 113-15,
115-19, 120, 245-46, 254
reinoculation of soil by bacteria, 13, 25,
113-15, 116, 253-54; without ammoni-
fiers, 13
Nitrifying bacteria, 13, 119, 239-40, 245; ef-
fect of pH on, 13, 120, 245-46; effect of
temperature on, 13, 115, 119, 121, 245-46;
inoculation in treated soil, 13, 25, 113-15,
116; sensitivity to soil treatment, 13, 95,
113-15, 115-19, 120, 245-46, 254
Nitrite, toxicity from, in soil, 121, 245
Nitrogen (Section 7), 108-22; also 105, 108,
110, 237
content in organisms, 242-44
conversion, 13, 245-46
cycle, 245-46; in soil, 109, 245-46; in plant,
109
deficiency, 1 8
essential to plants, 89, 106
fixed from air, 89, 244-45
fixing bacteria, 2 15
loss in organic matter decomposition, 65-67,
99, 100-1, 105-7
[ °>20 1
relation to damping-off, 42-43
starter solutions, 13, 14, 111-12, 254
tied up in soil by organic matter, 242-44;
by sugar, 243, 244
See also Ammonium; Fertilizer ingredients;
Fertilizers; Nitrate nitrogen; and Organic
nitrogen
Nitrobacter, 245
Nitrosomonas, 245
Nucleus block (mother block), 21, 31, 222,
235-36
Nursery industry in California (Section 2),
28-33
amount of soil used, 3, 29
climatic relations, 29-30, 233
decreasing returns, 32, 196
distance from market, 31-32
expanding local market, 31-32
future developments, 27, 193, 254
kinds of plants grown, 29
labor cost increasing, 32, 96, 196, 271
location in state, 28, 29
mechanization, see Mechanization in grow-
ing
moving to rural areas, 31-32, 274
number of units, 28
population pressure increasing, 31-32, 271,
274
production cost increasing, 31-32
real-estate development, 31, 271
rising land values, 31
size, 28-29, 33
smog injury, 31, 32, 274
tax rates increasing, 31, 271, 274
unit containers for marketing, 25, 31, 127
year-round growing, 3, 7, 30-31, 49
zoning restrictions, 31
Nursery Sanitation Code, 22-23
Nutrients for plants, availability affected by
microorganisms, 89, 237, 244-48; deficiency,
accumulative effect, 88-89; excess may kill
plants, 53, 54, 56-57, 64-65, 88-89
Nutrition research, only on healthy plants, 51
Oak leaves, 100
Oak-root fungus (Armillaria root rot), 135,
198, 220, 260-61
Objectives of manual, 4, 29, 33; microorgan-
isms included, 34
Obtaining pathogen-free planting stock, 219-
33
aging of seed, 21, 232
aseptic culturing of growing point, 20, 221
chemical treatment of stock, 20, 41-42, 230,
232, 236
continued roguing of stock, 21, 232, 300
cultured-cutting technique, 20, 221-22, 236
environmental control, 220-21
few healthy plants, 20, 219, 236
grow up away from soil, 20, 219-21, 236
heat treatment of stock, see Hot-water
treatment of planting material
indexing for viruses, 232-33
new seedlings, 233, 231, 236
sanitary practices, see Sanitary practices
select growing areas, 21, 233, 236
specialist propagator, 20, 31, 219, 233
tip cuttings, 20, 219-21
use of true seed, 21, 233, 234
Ocimum (sweet basil), 205
Odors from compost piles, 12, 90, 271; from
organic nitrogen, 122
Ohio soil heater (type 15), 165, 166, 177, 179,
195
Oil, fuel for boilers, 16, 136, 162, 163, 164-65,
174, 176, 185, 190, 192, 194
Oil-drum, method of soil steaming (type 12),
131, 164, 176
Oleander, stem and leaf gall, 220
Onion, stem and bulb nematode on, 258
Oospores, function in fungus carryover, 44-
45; occurrence, 44; useful in disease diag-
nosis, 44
Organic matter, 11, 104, 109, 120
carbon/nitrogen ratios, 242-44
decomposed by microorganisms, 89, 95, 115—
19, 237, 240-44
effect on aeration, 99; on microorganisms,
25, 238, 240, 242-44; on soil salinity, 15,
65-67
high-nitrogen materials, 243-44
low-nitrogen materials, 242-43
particle size, relation to soil leaching, 15,
65-67
rate of decomposition, 241-42
relation to aeration, 98-99, 120, 143, 149,
240; to steam penetration, 127-28
role in soil toxicitv, 95
shrinkage, 12, 85, 89-90, 100-1, 241
steps in decomposition, 241, 246-47
Organic nitrogen, 105, 108-9, 245
application rate, 13, 71-75
applied as top dressing, 13-14, 118-19, 121,
122
conversion in soil, 13, 53, 109, 112, 113, 245
effect of aeration on, 121; of chemical treat-
ment on, 119; of microorganism popula-
tion on, 108, 113, 120, 122; of moisture
on, 121; of quantity applied, on conver-
sion of, 117, 120; of steaming on, 94, 108-
9, 113-15, 115-19; of temperature on con-
version of, 13, 53, 105, 112, 115-19, 120
insoluble in water, 108
minimal nitrogen level supplied, 94, 121,
122
relation to ammonium injury, 13, 14, 95,
112, 113; to salinity, 70, 76'
relative rates of conversion. 13. 14. 118, 121
soil organisms converting, 13. 105, 245
unavailable to plants, 13-14, 108
[321]
Origin of plant, relation to distribution, 86,
91, 109
Orobanche, 261
Orthocide 406 (captan), 19, 43, 207, 209, 304
Osmotic concentration of soil solution, 95, 300
Overhead watering, 27; relation to disease
spread, 20, 23, 38, 39, 45; relation to salin-
ity burn, 9, 15, 53-54, 64
Oyulinia azaleae, 21, 30, 232, 233, 234
Owgen, 87, 121, 244, 298
Oystershell lime, 106
P-40 (sodium selenate), 232, 305
Package boilers, see Steam-generating equip-
ment
Pallet for stacking flats, 22, 25, 26, 166, 171,
174, 211, 212, 272-73, 276-77, 279, 280-81
Palms, 29, 284
Panics in nursery business, 7, 51
Pansy, 42, 43, 111, 207, 215, 264, 269
Papaver (poppy), 111, 215, 233
Paraformaldehyde, 19, 212-13
Parasite, 299, 300
Parasitic organisms in soil, attacking patho-
gens, 24, 238-40, 300; competition escape by
infecting plant, 21, 238
Parasitism, specialization, 5, 21, 46-47
Parathion, sources, 305; treatment of plant-
ing stock, 20, 232
Particle size, see Soil, compaction, and Soil,
drainage
Parzate (zineb), 267, 305
Pathogen, 127; definition, 300; depth in soil,
6, 120, 259; rate of increase, 218; soil-in-
habiting, 20, 218-19; sources, 123, 217; vari-
ability, 255-59
Pathogen-free planting stock (Section 13),
217-36; also frontispiece, 1, 6, 11, 19-20, 22,
24, 31, 34, 48, 111, 123; benefits from use,
49-51, 217, 218; importance, 7, 29, 31, 43,
217; maintaining, 21, 31, 226, 234-36;
methods of obtaining, 20, 21, 31, 41-42, 219-
33, 236, 300; obligation of nursery to pro-
duce, 6, 36, 262; report diseased stock to
propagator, 20, 233
PCNB ( 1 erraclor), 19, 43, 205, 207, 208-9, 305
Pea, 43, 215; Fusarium wilt, 257
Peach, root-knot nematode on, 259
Peanut, root-knot nematode on, 259
Peat, black (sedge), 69, 98, 265; source of sa-
linity, 15, 53, 98, 101-5; of soil toxicity, 95
Peat, hypnum, 69, 104
Peat, sphagnum, 12, 81, 91, 94, 97, 98, 99, 101,
104, 115-19, 112, 144, 228, 242, 268, 275, 276
buffering capacity, L06
cost, 69, 85, 100
cllcd on teachability of soil, 65-67
formation, 244
heal conductivity, 2!)!)
ingredient <>f l . C. type soil mixes, 72-75,
77, 78,81, 83-84, 85,93, 211
micronutrients, 107
mixing, 83-84
nitrogen content, 116, 244
pH, 69, 106, 120
seed cover for suppressing damping-off, 43
types, 69, 104
water retention, 69, 100
weight, 69
Pelargonium (geranium), 20, 21, 29, 32, 35,
215-16,221,234,261
Pelleting of seed, 25, 283
Pellionia, hardening for heat treatment, 223-
24; hot-water treatment, 229; Rhizoctonia
on, 220-21; U. C. system for, 267; water-
mold root rot, 220-21
Penicillin, 255-56; as a retardant, 25, 251-52;
effect of pH on, 251
Peperomia, Rhizoctonia on, 220; U. C. system
for, 267; water-mold root rot, 220
Pepper, 25-26, 29, 111, 214-15, 251-54, 256-57,
260, 264-65; heat treatment of seed, 226;
Phytophthora root rot, 258; Rhizoctonia in
seed, 25, 41-42, 43, 226, 260; root-knot nema-
tode on, 259; spotted wilt, 235
Perforated pipe method of soil steaming
(type 20), 16, 128, 131, 132, 138, 148, 150,
152, 156, 165, 166, 178, 180-83, 184, 194
Perlite, 12, 97, 100, 101, 227
Permeability of soil, 64—65; affected by clay
content, 143
Peronospora, 46-47
Persea (avocado), 45, 258
Persica (peach), 259
Petunia, 25, 207, 215, 264, 283; ammonium
injury, 13, 111, 112, 113; chlorosis, 113;
formaldehyde injury, 213; Rhizoctonia on,
43; Sclerotinia on, 46
pH, 95, 299, 300
desirable ranges for plants, 106
effect of peat on, 69, 106, 120
effect on ammonifiers, 120, 246; on con-
trolled colonization, 251; on nitrifying
activities, 13, 120-21, 245-46; on Peni-
cillium, 251; on soil microorganisms, 120-
21, 245-48; on Streptomyces, 251; on Tri-
chodcrma, 251
of U. C.-type soil mixes, 69, 70
relation to nutrient availability, 247
Phaseolus, see Bean and Lima bean
Philodendron, bacterial stem rot, 220, 229;
heat treatment of plants, 229, 231; Rhi-
zoctonia on, 220-21, 229; root-knot nema-
tode on; 259; II. C. system for, 267; water-
mold root rot, 220-21
Phlox, 111, 113, 261
Phomopsis, 233
Phosphorus and phosphate, 12-13, 70, 95,
106, 108, 110, 115; essential to plants, 89;
fixation, 77, 78; loss in organic matter de-
composition, 100; mono-ammonium phos-
phate, 11, 78; monocalcium phosphate, 70,
[322]
106; rendered available bv microorgan-
isms, 237, 247
Photosynthesis. 247
Phvcomvcetes. 301
Phyllosticta, 233
Phytophthora, 5, 7, 37, 44-46, 49, 82. 220:
capsici. 258; cinnamomi, 45-46, 218-19. 258;
parasitica f. nicotianae, 258, 261; richardiae.
229; variability in pathogenicity, 258
Pice a (spruce), 258
Pike's Peak plastic covering. 303
Pine. Pythium root rot, 258; Phytophthora
root rot. 46; shavings, 65-67, 244
"Pinto tag" in certification. 48. 129. 201
Pipe spacing in relation to steam flow rate.
130-31, 153, 180, 182
Pipe, steam-distributing. 195-96
Pisum <pea). 43. 215. 2"7
Plant, composition. 13s
Plant intioduction. ancient example. 91-93
Planter boxes. 131: fertilizer schedule. 81;
soil mixes. 81, 84
Planting depth, relation to damping-off, 5.
43
Planting equipment. 25-27. 264, 283, 302
Plastic containers. 53. 211. 212
Plicaria as a retardant. 25
Plow, steam. 182
Poinsettia. 29: Rhitoctonia on. 257; Thiela-
viopsis on. 258: U. C. svstem for, 266
Polvethvlene. 212. 213, 216, 221; sheets for
covering soil chemically treated, 201: for
steaming soil, 170. 178-80, 275. 303; under
flats on ground, 23, 41
Polyvinyl sheets, 201
Poppv. 111. 215; bacterial leaf spot, 233
Population pressure on nurseries, 31-32. 271,
274
Porosity of soil, see Soil porosity
Porous canvas hose, 303
Post-emergence damping-off, 5, 35-36, 249,
257
Pot filler. 25. 168, 272-73. 280, 282, 302
Pot plants. 169: fertilizer schedule. 80, 119:
soil mixes for. 12. 69. 73. 77. 79-80, 266-67:
U. C. svstem for. 266-67
Potassium and potash. 95. 99. 106, 108, 109,
110. 115: availability altered bv microorgan-
isms. 237. 247: contributes to salinity, 13;
essential to plant. 89, 106; frit. 76. 106; loss
in organic matter decomposition. 1
methods for mixing in soil. 70. 83-84, 105
Potassium chloride 14. 76. 77. 7V. 106. 305
Potassium nitrate. 13. 70-75, 94. 105, 106. 110,
111. 119. 177; mixing. 70, 105
Potassium sulfate 14, 53, 70-75, 76, 77, 91. 94.
106, 111, 119
Potato, Rhizoctonia on. 257; ring rot, 216:
scab, 247; virus X on. 221
Potato root nematode (Heterodera). lethal
temperatures. 139
Pothos, root-knot nematode on, 259
Pots. 126. 127. 150. 196. 210, 254, 272-73; salt
accumulation. 9. 15, 19. 53, 56, 211-12; treat-
ment. 15, 40, 162, 170, 171, 173, 201, 204,
211-16
Potting-on. soil mixes for. 71. 72. 73, 75, 119
Pounds of steam, 300
Pratxlenchus (lesion and meadow nemato<
47. 139. 227, 229
Preemergence damping-off, 5, 35-36, 249, 257
Preparation
of plant material for hot-water treatment,
20. 224
of U. C.-tvpe mixes, hand mixing. 83-84,
8; machine mixing, 83-84, 98, 276-79
Pressure cooker, see Autoclave
Pressureless steam, see Free-flowing steam
Pressure steam for soil treatment. 157, 158,
164-65, 167-74. 178-84, 301; advantages. 129.
158; disadvantages. 15-16. 129, 135; heat
content. 129, 157-58; pressureless in ^oil.
129. 149: thermal efficiency. 129. 157-58; see
also Autoclave and Equipment for soil
heating
Prevention, emphasized in plant disease. 6. 10,
48
Primula (primrose), soil mixes for. 79; Thie-
laviopsis on. 258
Production block (increase block . 222. 235-36
Production cost, reduction needed. 31-32
Propagating material, 29; pathogen-free, see
Maintenance of pathogen-tree stock and
Obtaining pathogen-free planting stock:
spread of pathogens. 6, 19-20. 29, 217:
treatment, chemical, 20, 42. 230. 232; treat-
ment, heat. 20. 164-65. 223-30, 236
Propagation operations, segregation from
commercial production, 21, 22-23
Propane, fuel for boilers. 162. 192. 195
Proportioners. for liquid fertilizer application.
283, 302: for Yapam application. 204
Protective seed treatment. 20-21. 42. 230, 232:
does not eradicate pathogens. 230
Protein. 241
Protozoa in soil. 21,238
P udomonas. 47
Pseudotsuga | Douglas Br), 46. 65-67
Psorosis, citrus. 232
Puratized Agricultural Spray, 228. 305
Purex isodium hypochlorite. 216. 221-22.
226. 305
Pythium, 5. 35, 37. 44-46. 205, 226-27: lethal
temperatures. 139; variability in parasitism.
258
Quantity of pathogens. 300; importance
42, 204. 260
Quantity of steam, calculation. 132-33: rela-
tion to soil volume and time. 132-33. 149-
52; required for soil treatment. 16. 159-60
[ 323 ]
Rack for steaming pots, 280, 282
Radiation of heat, 149, 159; definition, 141;
factors affecting in soil, 142; importance in
soil heating, 144, 150, 155; relation to pore
size, 144
Rainfall, free of salts, 15; relation to plant
distribution, 86
Rake method of soil steaming (type 21), 135,
148, 150, 165, 166, 178, 181, 183
Ranunculus, mosaic, 21, 233
Raphanus (wild radish), 235
Raspberry, crown gall, 258
Real-estate development, effect on nurseries,
31,271
Recontamination problem, 11, 20, 24, 93, 96;
balance in soil organisms, 21, 25, 238-40,
250-54; danger from inadequate soil treat-
ment, 22, 249-50; disease greatest from con-
tamination of treated soil, 20, 22, 249; effect
on organic nitrogen breakdown, 113-15,
120, 122; luxuriation of first contaminant,
22, 248-49; prevented by sanitation, 22-23,
250
Red stele of strawberry, 220
Redwood, used in soil mixes, fiber (bark), 98;
sawdust and shavings, 69, 81, 244
References, by section, 285-98
Relative humidity, 11, 15, 29-30, 42-43, 146-
47
Reliability of soil mixes, 68
Research use of U. C.-type mixes, 81-83;
makes possible the selection of uniform
plants, 83
Respiration, 87, 246-47
Retardant microorganisms, 4, 20, 21, 24-25,
27, 35, 113-115, 116,250-53, 254, 300
Returns, decreased, 32, 196; offset by reduced
competition, 32; offset by reduced produc-
tion cost, 32
Rhizoctonia diseases, 35, 38; see also Damp-
ing-off
Rhizoctonia solani, 5, 35, 37, 45, 46, 198, 214,
218, 220-21, 226-29, 231, 233, 239-40, 249-
50, 251-53, 266
aerial types, 256, 259
air-borne spores absent, 38
controlled by retardants, 25, 205, 207, 208
depth found in soil, 259
fungicides and inoculum potential, 260
increasing importance, 37, 12
lethal temperatures, 139
longevity in soil, 201
recognition in field, 38, 39
relation to Fusarium wilt of aster, 49-50;
to soil carbon dioxide, 259; to soil mois-
ture, 49-50; to temperature, 43, 259
saprophytic l<»i ms, 1 1, 257
seed i ransmission, 40-42
spread, 38-42
structure, 38, 39, II
subtei ranean i\ pes, 259
survival in soil, 38, 261
variation in host range and virulence, 38,
44, 256-57
Rhizoctonia "story," 38-44
Rhizomorph, 261
Rhizosphere, 240-41; definition, 240
Rhododendron, salinity injury, 58
Ribbon mixers, see Concrete mixers
Rice hulls, 12, 69, 80, 81, 97, 98, 267; potassium
content, 99-100, 267
Rock, 99
Roguing of planting stock, 21, 232, 300
Rollers, steel, 26, 272-75, 277, 279, 282
"Root action," 51, 138
Root distribution in U. C.-type mixes, 82-83
Root divisions unsafe for propagation, 22, 41-
42
Root functions, 51, 87, 89
Root injury, effect on plant responses to cul-
tural practices, 51; from ammonium, 13:
from drying soil, 268; from salinity, 8-9, 58-
60; from soil toxicity, 9, 113
Root-knot nematode (Meloidogyne), 47, 226-
27, 229, 233, 239, 261; lethal temperatures,
139; number of eggs laid, 218; obtaining
clean stock, 220; variability in pathogenicity,
258-59
Root lesion nematode (Pratylenchus), 47, 139,
227, 229
Root nodules on legumes, 245
Root rot, 34, 36-37, 202; Armillaria, 135, 198,
220, 260-61; Fusarium, 229, 256; Rhizoc-
tonia, 5, 256; Thielaviopsis, 258; water
mold, see Water-mold root rots
Root secretions, 259
Root tips, loss of, importance to plant, 51
Rose, 29, 35, 126, 268
chlorosis, 107
cultured-cutting technique with, 20, 221
dagger nematode on, 229
heat treatment of plants, 229
mosaic, 7, 21, 51,232,236
Rhizoctonia root rot, 43
root-knot nematode on, 229, 233
root-lesion nematode on, 229
spiral nematode on, 229
U. C. system for, 268
Verticillium wilt, 221,256
Rotating drum soil heaters, external flame,
batch type (type 35), 165, 191, 303; external
flame, continuous type (type 31), 165, 190,
273; internal flame (type 30), 165, 185, 187,
189-90, 191, 303
Rotating drum soil heaters, knife injector (type
28), 148, 165, 166. 185-87, 273; electric (type
33), 165, 189-90, 195
Rotating screw soil healers, external flame
(type 31), 165, 190; steam (type 29), 10, 165,
187-88,272. 303
Rubberized (loll) Eoi soil treatments. 178, 180,
182, L83
[ 324 ]
Rubus (raspberry and loganberry), 258
Ruckl method for soil steaming (type 1), 132,
148, 164, 166, 167-68, 180
"Running out," 235
Rust, snapdragon, incubation period, 231; in-
troduction to new areas, 218; number of
spores produced, 218
Saintpaulia, foliar nematode on, 232; salinity
injury to, 9, 53, 119
Salinity (Section 4), 52-67; also frontispiece,
1, 11,264,300
accumulation, in clay pots, 9, 15, 19, 53, 56,
211-12; in plant, 9, 55-56, 64; in soil sur-
face, 9, 55-56
dangerous level, 15, 61, 63, 65
definition, 52
deposit on leaves, 9, 63-64
differences in plant susceptibility, 7, 55, 61
injury to plants, see Salinity injury, below
leachate not good index of salts in soil, 65-
67
leaching soil to prevent, 9, 11, 14-15, 53-54,
57, 63, 65-67; effectiveness related to wa-
ter salinity, 9, 14, 63
measurement, 9, 14, 60-63, 84, 300
necessary to use excess water, 9, 14, 63
reduces available water, 87
relation to fertilizer application, 9, 15, 30,
52, 53, 57, 64-65, 70, 106, 119-20
role in soil toxicity, 9, 95, 98
safe levels, 61, 63, 65
selection of land to prevent, 64
soaking clay pots, 19, 53, 171-73, 211-12
sodium in water, 64
sources, 9, 30, 53-54, 70, 116, 275
use deionized water, 15, 57, 63-64
water quality, related to, 9, 11, 14, 30, 63-
64; characteristics, 63
Salinity injury, 1, 7-9, 55-56, 58-60, 87, 93,
121,265
aggravates Botrytis diseases, 8, 9, 46; damp-
ing-off, 5, 7, 9, 33, 42, 49-50, 55, 266
effect of bright sunlight on, 15, 55; of hu-
midity on, 15, 55; of organic matter on,
15, 65-67; of soil drainage on, 15, 53-54,
57, 64; of soil moisture on, 9, 11, 15, 33,
49, 53, 55-57, 64
from leaf absorption, 9, 15, 53-54, 64
from overhead sprinkling, 15, 53-54
humidifying to reduce, 55, 57, 64
reduced by U. C.-type soil mixes, 10, 15, 53,
64, 65-67, 90, 211, 265-66, 270
relation to plant distribution, 86
shading to reduce, 55, 57, 64
variable effects, 55, 58
Salts, see Salinity
Sand, coarse, 142, 144
aeration, 98, 143
determination in fine sand, 103-4
permeability, effect of clay on, 143
porosity, 143
retention of minerals, 99
seed cover for suppressing damping-oft, 4:>
specifications, 102-3
unsuitability for U. C.-type mixes, 68, 97
use, in J. I. composts, 91; in propagation,
126, 146, 184; in sand culture, 68
Sand, fine, for U. C.-type soil mixes, 12, 71-71,
77, 83-84, 93, 97, 101, 110, 264, 268
aeration, 98
availability, 12, 275
bacteria sparse in deep source, 13, 113-15,
240
buffering capacity, 106
content of coarse sand and of silt and clay,
12, 103
cost, 85, 100
determination of particle size, 103-4
gravel and sand quarries, source, 85, 97,
103-4
porosity, 143
retention of minerals, 99
sources, 85, 97, 103-4, 275
specifications, 12, 69, 101-4
unique ingredient of mix, 68
Sand culture, 68
"Sand snake," explained, 202
Sanitary practices, frontispiece, 1, 6, 11, 22-
23, 111, 123, 129,236,250
containers on ground, 6, 22, 23, 24, 41
covering containers, 6, 23, 41
degree of cleanliness required, 24
dipping cuttings in water, 5, 22, 38
discard flats with diseased seedlings, 22
glasshouse cleanup program, 213, 215
isolation house, 21, 23, 24, 234-35, 261
keep hose nozzle off ground, 5, 23, 24, 38-40
microorganisms of the same name, 23, 255-
62
overhead watering, 20, 23, 27, 38, 39, 45
pathogen-free stock, see Pathogen-free
planting stock
plant clean stock only in treated soil, 22, 48
removal of diseased parts, 21, 232
scattering dust in handling, 23, 41
segregate propagation activities, 21, 22-23;
treated from untreated containers, 22;
nursery operations, 21, 163, 166, 276
spattering soil in watering, 23, 24, 220
taking of cuttings, 22
treating, containers, 23, 24; floor before
dumping soil, 18, 22, 134, 166, 199; soil in
containers, 22, 126-27; tools, 19, 22, 23,
24, 40, 48, 201, 226
treating soil in containers, 22, 126-27
unnecessary handling of soil, 23
use treated containers for treated soil, 22.
210,278
walking over planted flats, 6, 23, 24, 40
washing hands, 23
Sanitation Code, 22-23
Sansevieria, chlorosis, 107
[ 325 ]
Saprophytes, 238-40, 300
Saprophytic organisms in soil, 238-40
Saturated-soil extract method for salinity
measurement, 61-63; comparison with dilu-
tion methods, 61; compensation for elec-
trode, 63; converting reading to ppm, 61;
description, 62-63; importance in salinity
measurement, 61; readings on U. C.-type
mixes, 65, 70, 266
"Saucepan" soil steamer, 176
Sawdust, 12, 69, 80, 81, 97, 98, 99, 100, 242-43,
244; cost, 85, 100; decomposition of, nitro-
gen required, 99, 242-43
Sderotia, 38, 39, 46, 300
Sclerotinia camelliae, 21, 232, 233, 234
Sclerotinia cottony rot, white blight, 5; con-
ditions favoring, 46; life history of causal
fungi, 46; number of spores produced, 218;
symptoms, 46-47
Sclerotinia minor, 5, 46
Sclerotinia sclerotiorum 5, 46; lethal tempera-
tures, 139
Sclerotium crown rot, 139, 226
Sclerotium rolfsii, 226; lethal temperatures,
139
Screening soils, 276-79
Screw-type soil treaters, see Rotating screw
Sedge peat, see Peat, black
Seed, infection of by Rhizoctonia, 41-42
Seed decay, 4, 35-36
Seed germination, relation to salinity, 9, 42,
55; soil mixes for, 74
Seed transmission, 6, 40-42, 217, 249, 255, 260;
Alternaria, 229, 233; bacteria, 229; Fusa-
rixim, 47; Phytophthora, 45; Rhizoctonia,
41-42, 260; Sclerotinia sclerotiorum and
minor, 46; Septoria, 226; viruses, 7, 21, 232-
34
Seed treatment
chemical, 230; eradicative, 230; protective,
20, 21, 42, 230, 232; protective, relation to
soil-inoculum potential, 42
heat, see Hot-water treatment of planting
material
Seed vitality and damping-off, 5, 43
Seeding, mechanical, 25-26, 264, 283, 302; com-
mercial use, 25, 264, 282; seed size in rela-
tion to, 25, 283
Semesan, 19, 207, 209; injury to roses, 207, 209;
injury to seedlings, 207; sources, 305
Senecio (cineraria), 1 1 1
Separator strips lor stacking Hats, 201, 279
Septoria late blight of celery, 21, 51, 226, 232;
number of spores produced, 21 H
Septoria leal spot of chrysanthemum, 233
Sewage sludge, 15
Shading ol plains, effecl on damping-off, 5,
42-43; on salinity injury, 15, 55
Shalil peach, 259
Shavings, wood, HO, HI, 97, 98, 99, 100, 242-43,
211, 268; (ost, loo; died on teachability,
65-67; require nitrogen in decomposition,
99, 242-43
Shepherd's purse seed, heat resistant, 139
Shredder for peat moss, 98, 276
Shrinkage of organic matter in composting,
12, 80, 85, 89-90, 97, 100-1, 241
Shrubs, 29
Silt, 97, 98-99, 104; determination in fine sand,
103-4
Sisalkraft cover for soil treatments, 178, 303
Skip-load tractor, 25, 84, 168, 272-73, 276, 278-
79, 280
Slugs, lethal temperatures, 139
Smog, injury, 31, 32, 274
Snapdragon, 25, 111, 207, 215, 263; ammonium
injury, 13, 113, 253; anthracnose, 233;
chlorosis, 113; damping-off, 47; downy mil-
dew, 46, 47; methyl bromide injury, 16, 18;
Phyllosticta leaf spot, 233; root-knot nema-
tode on, 259; rust, 218, 234
Snyder's plastic covering, for soil treatment,
303
Sodium, 64, 106, 109, 300; in water, related to
quality, 64, 106, 109
Sodium acetate, 112
Sodium hypochlorite, 216, 221-22, 226; sources,
305
Sodium nitrate, 105
Sodium oxalate solution, preparation, 103-4,
305
Sodium selenate (P-40), sources, 305; treat-
ment of planting stock, 232
Sodium sulfate, 65-67
Soft rot (bacterial), 21, 35, 226-27, 233, 235
Soil
absorption of water, gases, and salts, 95
analysis, 84, 99
clods, avoidance by U. C.-type mixes, 98,
133, 161, 276; relation to steaming, 15,
127, 133, 134, 140, 149, 160-61, 190
compaction, relation to fumigant move-
ment, 89, 142; to heat transmission, 130,
134, 142; to particle size, 97, 99, 103, 104,
142; to steam movement, 130, 134, 142,
H8-49, 152, 155, 156
conditioners, 15, 18, 65-67
drainage, relation to aeration, 60, 99; to
particle size, 97; to root rot, 44-45; to
salinity, 15, 53-54, 57, 64; restriction by
container boundary, 61, 87
drenches, see Spot treatment
functions for" plants, 10, 86-89
grinding of clods, 98, 133, 161
handling, separating various operations, 21,
163, 166, 276
heal capacity, compared with water, 133,
160
heal conductivity, 299
moisture, 29, 87-88, 120, 125, 300; effecl on
damping-off, 5, 33, .'50, 49-50; effect on
permeability, 143; effect on pore size, 1 13;
[326]
effect on soil steaming, 15, 130, 133, 131,
149, 155, 160, 193; high levels reduce
salinity injury, 9, 11, 15, 33, 49, 53, 55-
57, 64; relation to salinity measurement,
61; resulting from steaming, 135, 150-51;
see also Moisture, soil
nonspecificity for crops, 10, 86
particle size, in relation to concretion, 99,
103, 104, 142; see also Soil, compaction,
and Soil, drainage, above
permeability, 64-65, 143
porosity, effect of clay on, 99, 143; effect of
moisture on, 143, 149; in various soils, 98-
99, 143-44; porosity and pore size com-
pared, 143-44; relation to carbon dioxide
diffusion, 143; relation to convection
movement of steam and fumigants, 143-
44; relation to heat transmission, 141-44,
149
quantity used by California nurseries, 3, 29
relation to disease spread, 38, 45, 123, 217
relation to plant distribution, 86, 91
source of mineral nutrients, 89, 107
source of salinitv, 15, 30, 53-54
specific heat, 301
structure, 125
supplies most of plant requirements, 138
temperature, effect on ammonifiers, 121,
245-46; on damping-off, 5, 6, 43; on dis-
ease, 50, 260; on organic matter decom-
position, 53, 115-19
testing equipment, 303
top, cost, 85
weight, 135
See also Aeration of soil; Chemical treat-
ment of soil; Dry source of heat; Equip-
ment for soil handling; Hot-water treat-
ment of soil; Mechanization in growing;
Microorganisms, soil; Soil mixes, below;
Steam treatment of soil; and Toxicitv
after treatment of soil
Soil- and refuse-borne viruses, 127, 140
Soil mixes (sections 5 and 6), 68-107
conventional types, 91
Einheitserde, 94, 96
historv of development, 90-94, 110
ideal, 97, 109-10
John Innes composts, 91, 93
mix A, 12, 69,71, 77, 78, 85
mix B, 12, 69, 72, 77, 78, 79, 80, 81, 85, 111,
112, 115, 117, 135
mix C, 12, 69, 73, 77, 78, 79, 80, 81, 85, 149,
150, 153, 154, 156
mix D, 12, 69, 74, 77, 78. 80, 81, 85
mixE, 12,69,75, 77, 78,81,85
multiple vs. single mixes, 86. 89-90, 91
philosophies behind, 91, 93-94
U. C. type, 69-76, 93-94, 110; see also U. C.
type soil mixes
Solanum, see Eggplant and Potato
Soluble salts, see Salinity
Solubridge for salinitv measurement, 9, 60-
63, 299, 300, 303
Sore-shin damping-off (wire-stem;, 5, 35-36, 43
Sources, of equipment, 302-4; of fungicides
and chemicals, 304-6
Soybean, Rhizoctonia on, 257
Space in nurseries, reduced b\ U. C.-type soil
mixes, 10, 12, 89-90, 100
Specialist propagator, 20, 31, 219, 233
Specific heat, 301; of soil, 135; of water, 135;
of water vs. soil 15, 133, 131, 160, 196, 301
Spergon (chloranil), 230
Sphagnum peat moss, see Peat, sphagnum
Spike method for soil steaming (type 21), 135,
148, 150, 165, 166, 178, 181, 183
Spiral nematode (Helicliotylenchus), 229
Spore, 5, 46, 250, 298, 299, 301
Spot treatment, fungicidal, 19, 43, 48, 207,
209; application, 19, 207; importance of cor-
rect dosage, 207, 249-50; salvage technique,
19, 48, 207
Spotted-wilt virus, 21, 221, 235; endemic cen-
ters of infection, 235
Sprays, use, 4, 34
Spread of microorganisms, b\ :
air-borne spores, 5, 38, 46
cloth flat-covers, 6, 23, 41
containers, 5, 39-40, 45, 48
hormone solutions, 5, 22, 38
hose nozzle, 5, 23, 24, 38-40
placing container on ground, 6, 22, 23, 24,
41
planting material, 6, 19-20, 40-42, 43, 45-46,
48
seed, 6, 40-42, 45, 47, 217, 229, 233, 249, 255,
260
soil particles, 5, 38, 39, 48
tools, 6, 40-41, 45, 48, 217, 249
water, 5, 11,38,45,48
workers' hands or feet, 6, 23, 24, 40
Spruce, Pythium root rot, 258
Stacking of flats, for seed germination, 264; for
soil treatment, 131, 173, 189, 201-4, 211
Starch, 241
Started plants, 29
Starter solutions (nitrogen), 13, 14, 111-12, 254
Steady state in heat transmission, 145-46
Steam
box, for bulk soil (fixed front) (tvpe 4a), 16,
132, 148, 156, 164, 166, 167, 169-70, 176.
273, 303; for bulk soil and containers (re-
movable front) (tvpe 4b), 16, 17, 131, 132,
148, 156, 164, 166, 169-70, 303
B.t.u. requirements per cu. ft., 16, 159-60
calculation of volume required for soil treat-
ment, 132-33, 159-60
definition, 141
delivered, calculation, 301
differentiated from heat. 142
distribution, see Distribution system for
steam
[327]
Steam, continued
escape from treated soil, 128, 130, 131, 149-
50, 153, 155, 159-60
flow rate, relation to pipe spacing, 130-31,
153, 180, 182
forms, for soil treatment, 15-16, 129-30, 135,
149, 157-59, 164-65, 166, 196, 211, 300, 301;
equipment for generating, 191-92; for
specific types of soil-treating equipment,
167-74, 178-84, 187; with steam-air mix-
tures, 149
free-flowing, see Free-flowing steam or
Steam, forms of, above
heat content in various types, 156-57
movement, see Steam movement through
soil, below
pressure, see Pressure steam for soil treat-
ment or Steam, forms of, above
pressureless, from boiler, see Free flowing
steam; in soil, 129, 149, 158, 191
quantity of soil heated per pound, 16, 132-
33, 159-60
saturated, 300
specific heat, 301
superheated, see Steam, forms of, above
tunnel, 211
volume required for soil treatment, 16, 132-
33, 159-60
Steam-air mixtures in soil treatment, 127, 139,
148, 184
Steam/air ratio, and condensation, 146-48,
149-51, 152; relation to width of condensa-
tion zone, 146-49, 150, 152
Steam-chemical (type 26), 148, 165, 166, 184-
85,213
Steam-generating equipment, 191-95
boiler horsepower rating, 159-60, 193-94,
298, 300
boiler output, 298
built-in, 174-76, 184
cost, 135-37
distribution system, 129, 132, 136, 191, 194,
195-96, 299
flash steamers, 192, 302
fuel, 16, 135-36, 162, 163, 161-65, 174, 176,
177, 184, 185, 187, 190, 191, 192, 194-95
high vs. low pressure types, 191-92
modified from hot-water boiler, 192
package boilers, 302
portable unit, 168, 191
possible group-ownership, 193
regular boilers vs. flash steamers, 159, 192
size boiler required, I, 16, F32-37, 193-94
sources, 302
stationary <">. portable units, 163, 192, 193,
191
Buperheal vs. free-flowing vs. pressure types,
1 58-59
thermal efficiency, 191, 299
types ol boilers, 159, 192, 302
watei softeners, 192
Steam movement through soil, 149-51
atmospheric pressure of, 129, 149, 158, 191
condensation zone, 128, 146, 149, 150, 152
condensing capacity of soil, 149-52, 154-55
distance and flow rate are compensating,
130-31, 149-53, 156
effect of clods, 15, 127, 133, 134, 140, 149,
160-61, 190
expanding spheroid around outlet, 128, 131,
151, 152, 153-55
heat transferred by expelled air, 148, 150
movement through pores, 89, 149
relation to expanding volume of spheroid,
128, 153-55; to organic-matter content,
149; to soil compaction, 134, 142, 149, 155;
to soil moisture, 134, 149, 152; to soil
pores, 134, 148-49, 152
relative movement horizontally and later-
ally, 128, 153
steam-air mixture, 146-48
with high flow rate of steam, 152-53; inter-
mediate flow rate of steam, 152-53; low
flow rate of steam, 149-52
Steam treatment of containers, 19, 40, 111, 133,
134,211-12
Steam treatment of soil (sections 8 and 9), 123-
61; also frontispiece, 1, 11, 22, 48, 111, 123,
252, 254, 264, 280
advantages over chemicals, 1, 16, 18, 123-
25, 210; over dry heat, 125-26, 146
application to soil surface, 131-32, 170-76,
178-81, 184, 187, 188
balanced steaming, 130, 150, 155, 159-60;
methods of achieving, 159-60
batch methods, 133, 162, 166, 168, 191
benefits, 126
best done in containers, 15, 19, 48, 126-27,
164-65, 278
best treatment method, 15, 125, 197
"blow-out" from soil surface, 130-31, 149,
152-53, 155, 161
breakdown of urea-formaldehyde, 14, 118
bulk soil, 273
ceiling of 21 2°F, 125, 140
compaction of soil in relation to, 130, 134,
142, 148-49, 152, 155, 156
compared with chemicals, 1, 16, 18, 123-25,
210; with dry source of heat, 125-26, 146;
with hot water, 126, 1 16-18, 152, 156-57,
18 1
condensation process in soil, 128, 1 16, 119,
150, 152, 154-55
condensed water in steam line. 133, 152, 178,
196
conditions precluding steaming, 125, 133-
34, 1 18-19, 160-61
container size for chamber steaming, 131
continuous-batch equipment, 16, 166, 169,
171, 171, 176
cooling soil after treatment, 16, 134
cosl of, and iis calculation, is, 121, 135-37
| 328 |
depth of inputs in soil, 130-31
development, 138
effect on microorganisms, 113-15, 115-19,
120, 248-50; on soil structure, 126; on
watering practices, 7, 126
effectiveness, 16, 124; determination of, 121,
139
efficiency, different levels of, 135-36, 152,
159; factors in, 130-32, 149-53, 164-65,
194; measurement, 299
equipment for, see Equipment for soil heat-
ing
escaping steam, from chamhers, 130, 131;
from soil surface, 128, 149-50, 153, 155,
159-60
final temperature attained, 127, 128, 140, 163
flow rate, 130, 132-33, 149-55
impractical uses, 125, 133-34, 148-49, 160-61
in bulk, 162, 169; in containers, 162, 169,
272; in home vards, 36-37, 135, 193
in "pinto tag" certification, 48, 129
increased growth response, 126
injection into soil, 130-31, 153-56, 167-70.
180-81, 185-87
lumps of soil, effect, 15, 127, 133, 134, 140,
149, 160-61, 190
measurement of effectiveness, 125
moving soil mass, 16, 127, 140, 148, 162, 185-
91
objectives, 141
plow, 182
quantity of steam required, 132-33, 153-56,
159, 298
recommended time and temperature, mov-
ing soil, 127, 140; stationary soil, 128, 140
safe to use, 125
salinity from, 53, 264
settling of soil around steam pipes, 156
size of boiler required, 159-60, 194
soil leveled for treatment, 130, 155
soil moisture after treatment, 135, 150-51
soil moisture required, 15, 130, 133, 134, 149,
155, 160, 193
soil structure, effect on, 125; required, 15,
133, 160-61, 193
spacing of inputs in soil, 130-31, 134, 153,
155-56, 160, 180, 182; of steam pipes, 130-
31
stacking flats, 131, 189
stationarv soil mass, 16, 128, 132-33, 140,
162, 163, 166-77
steam-air-chemical mixtures, 125, 148
steam-air mixtures, 127, 139, 148
steam flow rate, most efficient, 130, 149-55
temperature, and time required, 15, 16, 113-
15, 124, 127-29, 139-40, 159, 163; in mov-
ing mass, 127; in stationary mass, 127;
measuring, 156
time, per cu. yd., 159, 194
toxicity, see Toxicitv after treatment of soil
"trickle finish," 128,130, 132, 155, 173
types of fuel, see Fuel for steam boilers
uneven heating, factors in, 133-34, 160-61
used in closed areas, 125, 210
used near living plants, 124, 125, 135, 210
. watering practices in treated soil, 125
weed control, 15, 126, 139-40
Steaming soil, equipment for, see Equipment
for soil heating
Steel, specific heat, 301
Steer manure, see Manure
Stellaria (chickweed), 235
Stem and bulb nematode [Ditylenchus), 47,
227; lethal temperatures, 139; variability
in pathogenicitv, 258
Stem and leaf gall, oleander, 220
Stem rot, 4, 35, 36; see also Damping-off
Stemphylium, 233
Stericover for soil treatments, 178, 303
Sterilite, for soil treatments, 303
Steriltex cover for soil treatments, 178, 303
Sting nematode (Belonolaimus), 261
Stock (Matthiola), 111, 215, 219, 263; am-
monium injury, 112, 113; bacterial blight,
218, 229, 261; Botrytis blight, 8, 9, 55; hot-
water treatment of seed, 229; mosaic, 235;
Rhizoctonia foot rot, 42, 43, 207; salinitv
injury, 7, 8, 9, 55, 58; Sclerotinia white
blight, cottony rot, 46; Verticillium wilt, 256
Stoddard solvent, sources, 305; toxicity to
plants, 215; used with copper naphthenate,
19,213
Stone-fruit viruses, 232
Storage of soil mixes, 13, 71-75, 275
Strains of a pathogen, determination, 6, 256-
59; differences between, 6, 43; effects on
disease, 6, 256-59; relation to pathogen-free
stock, 43
Strawberry, 220
Strelitzia, 229
S:reptom\ces as a retardant, 25, 251; effect of
pHon,251
Streptomycin, 255-56
Stunting of plant, from salinity, 8, 42, 55;
from soil toxicitv, 9, 79, 95, 111
Subirrigation, relation to salinitv, 63, 119, 183
Substrate, 301
Succulents, 20, 29, 37
Sugar, 241
Sid fate in water, 64
Sulfate of potash, see Potassium sulfate
Sulfur, bacteria, 246-47; evele, 246-47; essen-
tial to plants, 89, 106; rendered available by
microorganisms, 237, 246-47; soil acidifi-
cation, 246-47
Sulfuric acid, 247
Summary, general (Section 1), 3-27
Superheated steam, 16, 135. 211. 301; advan-
tages, 130, 158-59, 166; equipment for gen-
erating, 192; heat content, 130. 157-59, 166;
thermal efficiency. 130, 157-59; see also
Steam, forms of soil treatment
[ 329 ]
Supernatural cause of disease, 3, 34
Superphosphate, single and double, 14, 70-75,
76, 77, 91, 94, 106;\reble, see double, above;
use finely ground product, 70
Support, as a soil function, 10, 87
Suppression of damping-off is not control, 6,
23, 36-37, 43-44, 45
Surface application of organic fertilizer, ad-
vantages, 13-14, 119, 121, 122; disadvantages,
122
Surface methods of soil steaming, 131-32, 170—
76, 178-81, 184, 187, 188
Survival of microorganisms in soil, 21, 238,
243, 261
Susceptibility of host, to ammonium injury,
13, 96, 111, 112, 115; to damping-off, 5, 42;
to disease, 5, 300; to nematodes, 258-59; to
root rot, 256-58; to salinity, 7, 55, 61
Sweet alyssum (Lobularia), 13, 111, 112, 113,
264
Sweet basil, 205
Sweet pea, seed decay, 230
Sweet potato, 221
Syngonium, black cane rot, 229; hot-water
treatment of plants, 227, 229-30; effect on
dormancy, 229-30
Systox (Demeton), 232, 304
Tagetes, starter-solution tests, 111; Rhizoc-
tonia on, 256
Tanks, hot- water- treating, 302
Tax rates increasing, effect on nurseries, 31,
271,274
Tear gas, see Chloropicrin
Temperature, 29; lethal to microorganisms
and weeds, 127, 139-40; recommended for
soil steaming, 15, 16, 113-15, 124, 127-29,
139-40, 159, 163; relation to plant distribu-
tion, 86; relation to variability of micro-
organisms, 259; see also Tempil pellets and
Thermometers
Tempil pellets for temperature measurement,
129, 156, 303
Terraclor (PCNB), 19, 43, 205, 207, 208-9; ef-
fectiveness, 205; sources, 305; specificity, 205
I ersan (thiram), 19, 43, 207, 209, 305
Thermometers, 128-29, 156, 302; expanded-
scale type, 225, 302; precision type for check-
ing those used, 224-25, 302; see also Tempil
pellets
Thielaviopsis basicola, variability of patho-
genicity, 258
Thiram (Arasan, Tersan), 19, 43, 207, 209;
sources, 305
I hornas method lor soil steaming, 163; effec-
tive depth, 131, 178; equipment, 178-79;
for beds or benches (surface) (type 18), Hi,
131, 132, 11H, 163, 165, 166, 171, 178-80;
movable variant, 118, Kit;, 180; lor contain-
ers (type ")), Hi, 131, 132, 118, 164, 166, 170-
71, 179,272
I hrips, 'J
Tip cuttings to eliminate pathogens, 20, 219-
21
Tipburn, salinity, 8-9, 55, 58, 60
Tobacco, 82, 214, 215, 248; mosaic, 140; Phy-
tophthora root rot, 258, 261; Thielaviopsis
on, 258
Tomato, 25-26, 29, 111, 260, 264-65; broom-
rape on, 261; crown gall, 258; Fusarium wilt,
257; Rhizoctonia on, 41, 42, 256; root-knot
nematode on, 259; spotted wilt, 235; Verti-
cillium wilt, 256
Tools, relation to spread of pathogens, 6, 40-
41, 45, 48, 217, 249; treatment, 19, 22, 23,
24,40,48, 201,226
Top rot of seedlings, 4, 35, 37, 38
Toxicity after treatment of soil, frontispiece,
1,9-11,90,93,98, 124, 140
caused by ammonium, 9, 13-14, 79, 95, 96,
98, 111-13, 115, 121, 122, 199, 253-54; by
manganese, 9, 95, 98; by other agents, 95;
by salinity, 9, 95, 98; by soluble organic
matter, 9-10, 95, 98
effects on plants, 9, 94-95
factors affecting type and severity, 94
persistence, 95
reduction by aging soil, 10, 93, 95, 96; by
immediate planting, 10, 95, 96; by leach-
ing soil, 10, 95, 96; by steaming ingredi-
ents separately, 93; by using U. C.-type
mix, 9-10, 11, 12, 15, 90, 93, 96, 97-98,
124, 129, 140, 199, 270
residue of chemicals, see Chemical residue
Transit mixers, see Concrete mixers
Transpiration, 54—55, 56-57, 87
Transplanting, 25, 81, 264, 282-83
Transplants, soil mixes for, 71, 72, 74
Treated soil, see Chemical residue; Recon-
tamination problem; and Toxicity after
treatment of soil
Treatment, see Chemical treatment of soil;
Containers, treatment of; Dry source of
heat for soil treatment; Hot-water treatment
of soil; Obtaining pathogen-free planting
stock; Steam treatment of soil; and Tools,
treatment
Trees, 29
Trichoderma as a retardant, 25, 240, 251-52;
effect of pH on, 251
"Trickle finish" in soil steaming, 128, 130, 132,
155, 173
Trifolium (clover), 259
Triton B-1956, spreader, 232, 305
Tropaeolum (nasturtium), 215, 224, 235
"Trough" soil steamer, 176
Tub containers, 131
Tubular soil heater with electric elements, 177
l ufedge (over for soil treatments, 178, 303
lung, Rhizoctonia on, 257
linl, for soil mixes, 91, 93, 110; source of
composl variability, 10. 89; unavailability,
12,90, 93
| 330 |
I'.C.L.A. blend, 93; see also U. C.-type s:»ii
mixes
U. C. system (Section 1), 3-27; also frontis-
piece,'27, 123; advantages, 1, 3, 30-33, 49,
51, 270; aids in adopting, 1-2; explanation,
3, 4; grower experience, 263-70; mechani-
zation, 271
U. C.-type soil mixes (sections 5, 6), 68-107;
also frontispiece, 1, 10-13, 93-94, 123, 197
adoption, 1-2, 27, 79, 263-64
advantages, 1, 10-12, 89-90, 93-94, 96, 265,
270
aeration, 87, 270
application to bench and bed crops, 12, 69,
80-81, 268; to can plants, 69, 72, 80, 267;
to cvmbidiums, 268-69; to flatted plants,
12, 69, 72, 75, 79, 264-65; to foliage plants,
20, 29, 32, 266-67; to home-yard planting,
81; to planter boxes and dish gardens, 81,
84; to pot plants, 12, 69, 73, 77, 79-80,
266-67; to research, 81-83; to vegetable
plants, 265-66
base exchange, 99
centralized soil service, 193
components, see Ingredients for U. C.-type
mixes
composting eliminated, 89-90, 93, 270
conductance, 65, 70, 266
cost, 12, 69, 80, 84-85, 100
cultural practices modified by use, 27
development, 93-94, 110
dump soil, re-use, 84
enable scheduled production, 94
evaluation, 263-70
facilitate mechanization, 25, 90, 94, 270, 271
fertilizers included in mixes, 69-76; see also
Fertilizer ingredients
fertilizing, see Fertilizers, dry, and Fertili-
zers, liquid
formulas, 76-79
leachabilitv, 65-67
micronutrients, 12, 89, 101, 106-7, 109, 110
mixes A to E, 69-76; see also Soil mixes
mixing, 83-84, 97, 98, 105, 133, 276-79
moisture retention, 12, 69, 87, 97, 100, 270
nontoxicity after treatment, 9-10, 11, 12, 15,
90, 93, 96, 97-98, 124, 129, 140, 199, 270
permeability, 64-65
pH, 69, 70
plant growth, 27, 265-66, 270
preparation, 83-84, 97, 98, 105, 133, 276-79
reduce labor, 10, 84, 89-90, 100, 270; space
requirement, 10, 12, 89-90, 100; odor and
fly problems, 12, 90,271
reliability, 68, 270
reproducible, 10, 89-90, 93
retention of nutrients, 12, 97, 99
root distribution in, 82-83
salinity problem reduced, 10, 15, 53, 64, 65-
67,90,211,265-66,270
shrinkage in storage, 12, 80
transplanting to clay soil, 81
types planted within a week, 71-75, 275, 278
types stored before use, 13, 71-75, 275
uniform initial fertility, 12, 98-100
uniform materials, 12, 97-98
uniform results, 12, 68, 89-90, 270
uses, 12, 69, 79-83, 264-70
variants, 69-76, 93
water content, 12, 69, 87, 97, 100, 270
watering, 27, 81; adjustment when first us-
ing, 79, 84
weight, per cu. ft., 12, 69, 80
Ultron cover for soil treatment, 302
Uneven soil heating with steam, causes, 134
Unit containers for marketing, 25, 31, 127
Unsteady state in heat transmisison, 145-46
Urea, 13, 14, 78, 79, 105, 106, 108, 109, 118, 245
Urea-formaldehyde resins, 13, 14, 79; biuret
content, 13, 14, 78, 79, 119; effect of steam-
ing, 14, 118; use as fertilizers, 105, 115-19,
121
Vacuum-plate seed planters, 25-26, 264, 283,
302
Vapam, 18, 204-5, 208; application, 18, 204-5;
effectiveness, 204; sources, 305
Variability of pathogens, 255-59
Vault for soil steaming (type 6), 16, 25, 131,
132, 148, 164, 166, 167, 171-72, 174, 272, 277,
280-81
Y-C 13, 206, 305
Vegetable plant production, 29, 129; U. C.
system for, 111, 264-66
Velon Fumicover for soil treatments, 178, 180,
303
Venturi tube, in steam-air mixing, 148
Verbena, 86, 11 1, 1 13, 264
Vermiculite, 12, 94, 97, 100, 101
Vertical cabinet for soil steaming (type 8), 131.
132, 148, 164, 166, 173-75, 176; self-generat-
ing type, electric (type 11), 131, 164, 174,
175-76, 195
Verticillium albo-atrum, 198, 220, 222, 239-40,
250; survival in soil, 261; variability of para-
sitism, 256
Verticillium wilts, 7, 18, 31, 49, 201, 203, 219,
235; cultured-cutting technique against.
221-22; ineffectiveness of methyl bromide
against, 16, 18, 22, 124, 203
Vigna (cowpea), 95
Yinca, 111
Viola, see Pansy and Violet
Violet, 263
Virulence of pathogens, 5, 6, 260, 300; varia-
bility in. 256-59
Viruses, 299; elimination by culturing grow-
ing point, 221; elimination by use of true
seed, 7, 21, 232-34; inactivation by soil heat-
ing, 140; indexing, 232-33; survival in
refuse, 140; survival in soil, 140
Viscosity, of gases, 143; of steam, 143
[331]
Visqueen cover for soil treatments, 178, 201,
302, 303
Volatilization of chemicals for soil treatment,
148, 165, 166, 184-85,213
Volume of steam, 16, 132-33, 149-52, 159-60
Water
application by porous hose or drip system,
81
calcium and magnesium content, 64
changes form at different temperatures, 156
conductance, 9, 14, 63
deficit, cumulative effect on plant, 87-88
deionized, 15, 63-64
heat conductivity, 299
leaching with, see Leaching to reduce sa-
linity
loss by transpiration, 54-55, 56-57, 87
necessary to use excess, 9, 14, 63
organisms spread in water supply, 5, 11, 38,
45,48
quality, in relation to salinity, 9, 11, 14, 30,
63-64; characteristics, 63
retention by U. C.-type soil mixes, 12, 69,
87, 97, 100, 270
salt deposit on leaves from, 9, 63-64
sodium content, 64, 106, 109
solvent for minerals, 87
source, of micronutrients, 107; of salinity,
9, 11, 30,53-54, 192
specific heat, 301
supplied by soil, 10
use in plant metabolism, 87
Water breakers on hoses, 84
Water-culture growing of plants, 87
Water-mold root rots, caused by Pythium
and Phytophthora, 7, 35-36, 43, 44-46, 49-
50, 82, 135, 139, 220, 226-27, 229, 233, 235,
250, 261; favored by very wet soil, 36, 43,
44, 49-50; symptoms, 35-36, 44-45; see also
Damping-off
Water molds, 5, 22, 38, 49-50, 220-21, 238,
301; lethal temperatures, 139; life history,
44-45; retard root development, 45; sur-
vival in soil, 261
Water requirements of plants, 51, 87
Water softeners, for boilers, 192; unsuitable
lor plant use, 64
Water spotting, 9, 63-64
Water trap in steam lines, 133, 196
Watering of plants, in steamed soil, 126; in
U. C.-type mixes, 27, 79, 81, 84; mechan-
ized, 27, 283-84; relation to disease, 43, 49
Watermelon, root-knot nematode on, 259
Weed hosts of viruses, 235, 275
Weed killers, 18
Weeding in containers, cost of, 126, 264;
elimination by soil treatment, 126, 264-65,
269-70
Weeds, 261, 264, 275; control by soil treat-
ment, 15, 18, 124, 126, 138, 197, 198, 200,
202-3, 204, 208, 248; lethal temperatures
of seed, 127, 139-40
Weigelia, hot-water treatment of plants, 229;
root-knot nematode on, 229
Weights, table of, 301
Wheat straw, 100, 254
Wheatstone bridges, see Solubridge for sa-
linity measurement
White blight, see Sclerotinia cottony rot
Wild-oat seed, heat resistant, 139
Wild radish, stock mosaic, 235
Wilting, plant, 87; root rot, 36; salinity in-
jury, 9, 55
Wire-stem damping-off, 5, 35-36, 43
Wolman salts for wood preservation, 215, 216
Wood, specific heat, 301
W^ood shavings, see Shavings, wood
Woody plants, can-grown, U. C. system for,
69, 72, 80, 267
Worms, lethal temperature, 139
Xiphinema (dagger nematode), 229
Year-round growing, 3, 7, 30-31, 49; under
glass, 7
Zantedeschia, see Calla
Zea (corn), 240-41
Zinc, 95, 237; essential to plants, 89, 106; role
of microorganisms in deficiency of, 248
Zineb (Parzate), 267; sources, 305
Zinnia, 111; Alternaria disease, 218, 229, 233;
hot-water treatment of seed, 229; Rhizoc-
tonia in seed, 42, 229
Zoning restrictions against nurseries, 31
Zoosporangia, 44-45
Zoospores, 44-45
Cooperative Extension work in Agriculture anil Home Economics College .,( v n. uJiure, University of California, and United Statei Department of Agriculture
co operating. Diatribuled In IuiiIhi.hu.- of tin- ,\< i <>i < <m; >. ..( May h, un.l Jon.- 30, 1914 George 1!. Alcorn, Director, California Agrii ultural Extei Service.
lm •<::>!< B8163 ;.\lk
E ON THE LAST DATE
"D BELOW
No matte lat kill , Ac THER BORRQ, tave . . .
... if you employ usual nursery pr CT1ER ONE Wfs, this manual shows you how to
cut your costs and losses, and incre 'O
The nursery program it offers
can help you to cut— maybe even eliminate— losses from diseases and weeds, and at the
same time cut the cost of fighting them! The program is the result of 16 years' research
by the Department of Plant Pathology, University of California, Los Angeles. The
methods have been thoroughly tested in commercial nurseries, not just in the laboratory.
The U. C.-type soil mixes
are basic to the program. Besides, they offer you worth-while savings in labor costs
and storage space, not to mention surer and probably faster results.
Mechanizing your operations
can further cut labor costs. With an effective disease-prevention program and a U. C.-
type soil mix, mechanizing has become a fact. The manual describes mechanization as
it has developed in a number of California nurseries.
IK
Your nursery is unique. **"
Your problems are somewhat different from anyone else's. |VA nursery business in
California is a varied one, and no rules of thumb will applf'to all the hundreds of
crops grown here. Neither will detailed directions cover all future developments in the
industry. Therefore the manual presents a general program, explains the facts behind
it. It gives many down-to-earth examples. It describes and illustrates the various kinds
of equipment you might use. With this background and the knowledge of your prob-
lems, the program can be adapted to your needs, now and in the future.
For your convenience, nn
references where you can find still further information on specific points, a glossary,
some methods of computation, a table of weights and measures, and sources where
you can get equipment and materials are given in an appendix. An index is provided
for rapidly locating information.
,,*'■ ' -
To obtain additional copies of this manual or a catalog listing other manuals arid free publica-
tions, see your University of California Farm Advisor (offices located in most California counties),
or write to:
Agricultural Publications
22 Giannini Hall
University of California
Berkeley 4, California
When ordering manuals, send orders and payment to the address above; make checks or money
orders payable to The Regents of the University of California.